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  <idinfo>
    <citation>
      <citeinfo>
        <origin>Arthur J Merschat</origin>
        <origin>Gregory J Walsh</origin>
        <origin>Peter M Valley</origin>
        <origin>Ryan J McAleer</origin>
        <origin>Thomas R. Armstrong</origin>
        <origin>Ernest A Crider</origin>
        <pubdate>20250516</pubdate>
        <title>Database for the bedrock geologic map of the Bellows Falls 7.5- x 15-Minute Quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire</title>
        <geoform>vector digital data</geoform>
        <serinfo>
          <sername>Scientific Investigations Map</sername>
          <issue>3535</issue>
        </serinfo>
        <pubinfo>
          <pubplace>Reston, Virginia</pubplace>
          <publish>U.S. Geological Survey</publish>
        </pubinfo>
        <othercit>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000, https://doi.org/10.3133/sim3535</othercit>
        <onlink>https://doi.org/10.5066/P172BBFC</onlink>
        <lworkcit>
          <citeinfo>
            <origin>Arthur J. Merschat</origin>
            <origin>Gregory J. Walsh</origin>
            <origin>Peter M. Valley</origin>
            <origin>Ryan J. McAleer</origin>
            <origin>Thomas R. Armstrong</origin>
            <pubdate>2025</pubdate>
            <title>Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire</title>
            <geoform>publication</geoform>
            <pubinfo>
              <pubplace>n/a</pubplace>
              <publish>US Geological Survey</publish>
            </pubinfo>
            <onlink>https://doi.org/10.3133/sim3535</onlink>
          </citeinfo>
        </lworkcit>
      </citeinfo>
    </citation>
    <descript>
      <abstract>The bedrock geology of the Bellows Falls 7.5 x 15 minute quadrangle, Vermont and New Hampshire, consists of polydeformed Ordovician to Devonian metasedimentary, metavolcanic, and metaplutonic rocks of the Connecticut Valley trough, Bronson Hill anticlinorium (or Bronson Hill terrane), and the Central Maine terrane. Previous work in this area includes a 1:62,500-scale published map and text by Kruger (1946), state geologic maps of New Hampshire (Lyons and others, 1997) and Vermont (Ratcliffe and others, 2011), and various maps and reports presented largely as parts of field trip guidebooks (e.g., Thompson and Rosenfeld, 1979; Chamberlain and others, 1988; Spear, 1992; Thompson and others, 1993). Armstrong (1997) completed a provisional open-file map of the geology of the Vermont part of the Bellows Falls 7.5 x 15 minute quadrangle, which is incorporated and revised on this map based on additional field work. 

This study recognizes three major structural levels from west to east, lowest to highest: (1) autochthonous rocks of the Connecticut Valley trough (CVT); (2) allochthonous rocks of the New Hampshire sequence and Bronson Hill arc in the Monroe thrust sheet, including the Skitchewaug nappe; and (3) allochthonous rocks of the Fall Mountain thrust sheet or nappe. The CVT consists of metasedimentary and metavolcanic rocks of Devonian Gile Mountain and Waits River formations, which are located west of, and within splays of the Westminster West fault zone. The CVT rocks are largely greenschist facies with most rocks in the biotite to garnet zones. The Monroe thrust sheet carries transported New Hampshire sequence, and include rocks previously described as the Cornish and Skitchewaug nappes (Thompson and others, 1968), and now interpreted to be largely at the same structural level (Walsh and others, in press). These rocks reached greenschist to amphibolite facies, with the lower biotite grade rocks occurring to the west near the Connecticut River. The eastern side of the CVT and the western side of the Skitchewaug nappe are dissected and deformed by multiple strands of the sinistral Westminster-West fault (Armstrong, 1997; McWilliams and others, 2013), an Alleghanian structure. The largest strand is marked by a significant zone of phyllonites—derived from various adjacent rock types from within the CVT—and chlorite grade retrogression. In the fault zone west of the Connecticut River, higher grade metamorphic assemblages are retrograded, deformed, and truncated in this wide zone. The Skitchewaug nappe shows an internal west-to-east increase in metamorphic grade from garnet zone to staurolite zone to sillimanite + muscovite zone near the Alstead dome. The Skitchewaug nappe exposes Ordovician to Devonian rocks of the New Hampshire sequence: Ordovician Partridge Formation, Silurian Clough Quartzite, Silurian Fitch Formation, and Devonian Littleton Formation. The Alstead dome is cored by Ordovician Ammonoosuc Volcanics and intruded by Oliverian Plutonic Suite trondhjemitic to granitic gneisses. The Ammonoosuc Volcanics is comprised of various amphibolites and hornblende schists. A metatuff mapped at the top of the Ammonoosuc Volcanics along the western flank of the dome yielded a Sensitive High Resolution Ion Microprobe (SHRIMP) U-Pb zircon crystallization ages of 455 ± 11 (Merschat and others, 2015; Valley and others, 2015, in press). Gneisses of the Oliverian Plutonic Suite are separated into two bodies: a smaller body to the north (~1.5 km long) and larger body extending southward beyond the quadrangle border. SHRIMP U-Pb zircon crystallization ages from these bodies are 448 ± 7 Ma and 452 ± 6 Ma, respectively (Merschat and others, 2015; Valley and others, 2015, in press). Map-scale truncations, a metamorphic break (staurolite against biotite and garnet zones), and mylonitic fabrics indicate a fault along the west side of the Skitchewaug nappe, which is mapped as the Northey Hill thrust. The structurally highest nappe, Fall Mountain, is floored by the Brennan Hill thrust (BHT) and contains sillimanite zone and higher-grade Silurian Rangeley Formation intruded by the ~400 Ma Bethlehem Granodiorite (Merschat and others, 2015). The BHT truncates units of the Skitchewaug nappe and juxtaposes the Bethlehem Granodiorite and migmatitic, sillimanite + K-feldspar zone Rangeley Formation over staurolite zone rocks of the Skitchewaug nappe. Reduction in grain size and an increase in the amount of biotite and muscovite in the Bethlehem Gneiss occur near the BHT. Mineral lineations plunge southeast, and kinematic indicators and fold patterns support NW-directed transport. The Fall Mountain nappe may be a west-directed sheath fold, similar to the Skitchewaug nappe and other F1-nappe stage folds (Walsh and others, in press).

40Ar/39Ar muscovite and amphibole ages across the nappes suggest Devonian to Mississippian cooling of the Bronson Hill anticlinorium. Amphibole from the Skitchewaug nappe in a window through the Fall Mountain nappe yields the oldest age at ~380 Ma, while amphibole age spectra from the Alstead dome yield ages of ~330 Ma. Muscovite ages from the Fall Mountain nappe and the Littleton Formation in the Monroe nappe in Vermont yield ages of 316-335 Ma, while ages near the Alstead dome are younger, ~300 Ma. Collectively, the 40Ar/39Ar data suggest peak metamorphism in the Skitchewaug nappe prior to ~380 Ma followed by emplacement of the FM between 335–380 Ma. The Alstead dome may have formed at ~330 Ma or later, and local late fabrics and younger muscovite ages are probably related to late Alleghanian sinistral tectonics. 40Ar/39Ar muscovite ages from the Westminster-West fault zone indicate it is a sinistral Alleghanian fault at ~300 Ma (McWilliams et al., 2013).

Extensional Mesozoic faults cut all structural levels. Mesozoic faults have normal dip-slip and strike-slip kinematics. Apatite fission track (AFT) data indicate that the brittle Ammonoosuc fault was active prior to about 100 Ma and experienced little to no re-activation in the Cretaceous, but other regionally significant older ductile faults such as the Northey Hill experienced late Cretaceous (less then 80 Ma) re-activation (Roden-Tice and others, 2009).  Additional AFT data suggest some Cretaceous activity on regional brittle faults like the Grantham fault may have extended into the Paleocene (Schnalzer and others, 2015). Extensive brittle faults and slickensided foliation surfaces in the vicinity of the Westminster-West fault zone, especially along Interstate 91, attest to Mesozoic re-activation of earlier structures.</abstract>
      <purpose>The bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle is intended to serve as a foundation for applying geologic information to problems involving land use decisions, groundwater availability and quality, earth resources such as natural aggregate for construction, assessment of natural hazards (earthquakes), and engineering and environmental studies for waste disposal sites and construction projects.</purpose>
      <supplinf>BellowsFallsNHVTSIM3535.gdb is a composite geodataset that conforms to "GeMS (Geologic Map Schema)--a standard format for digital publication of geologic maps, version 2.0", available at http://ngmdb.usgs.gov/Info/standards/GeMS/. Metadata records associated with each element within the geodataset contain more detailed descriptions of their purposes, constituent entities, and attributes. Two shapefile versions of the dataset are also available. The OPEN shapefile version consists of shapefiles, DBF files, and delimited text files and retains all information in the native geodatabase, but some programming will likely be necessary to assemble these components into usable formats. The SIMPLE shapefile version consists only of shapefiles and is easily used, but lacks some information present in the native geodatabase.</supplinf>
    </descript>
    <timeperd>
      <timeinfo>
        <sngdate>
          <caldate>20250601</caldate>
        </sngdate>
      </timeinfo>
      <current>publication date</current>
    </timeperd>
    <status>
      <progress>Complete</progress>
      <update>None planned</update>
    </status>
    <spdom>
      <bounding>
        <westbc>-72.5012</westbc>
        <eastbc>-72.2483</eastbc>
        <northbc>43.2516</northbc>
        <southbc>43.1235</southbc>
      </bounding>
    </spdom>
    <keywords>
      <theme>
        <themekt>ISO 19115 Topic Category</themekt>
        <themekey>geoscientificInformation</themekey>
        <themekey>environment</themekey>
      </theme>
      <theme>
        <themekt>USGS Thesaurus</themekt>
        <themekey>radiometric dating</themekey>
        <themekey>uranium-thorium analysis</themekey>
        <themekey>potassium-argon analysis</themekey>
        <themekey>uranium-lead analysis</themekey>
        <themekey>maps and atlases</themekey>
        <themekey>geologic maps</themekey>
        <themekey>earth sciences</themekey>
        <themekey>cartography</themekey>
        <themekey>geology</themekey>
        <themekey>economic geology</themekey>
        <themekey>geochronology</themekey>
        <themekey>petrology</themekey>
        <themekey>stratigraphy</themekey>
        <themekey>structural geology</themekey>
        <themekey>geologic processes</themekey>
        <themekey>metamorphism (geological)</themekey>
        <themekey>tectonic processes</themekey>
        <themekey>deformation (geologic)</themekey>
        <themekey>folding (geologic)</themekey>
        <themekey>fracture (geologic)</themekey>
        <themekey>faulting (geologic)</themekey>
        <themekey>geologic history</themekey>
        <themekey>geologic structure</themekey>
        <themekey>foliation (geologic)</themekey>
        <themekey>lineation (geologic)</themekey>
        <themekey>rocks and deposits</themekey>
        <themekey>igneous rocks</themekey>
        <themekey>volcanic rocks</themekey>
        <themekey>plutonic rocks</themekey>
        <themekey>metamorphic rocks</themekey>
        <themekey>bedrock geologic units</themekey>
        <themekey>geologic contacts</themekey>
        <themekey>natural resource extraction</themekey>
        <themekey>mining and quarrying</themekey>
        <themekey>geologic time periods</themekey>
        <themekey>Mesozoic</themekey>
        <themekey>Cretaceous</themekey>
        <themekey>Paleozoic</themekey>
        <themekey>Silurian</themekey>
        <themekey>Ordovician</themekey>
        <themekey>Devonian</themekey>
        <themekey>Permian</themekey>
      </theme>
      <theme>
        <themekt>Geologic Names</themekt>
        <themekey>White Mountain Igneous Suite</themekey>
        <themekey>New Hampshire Plutonic Suite</themekey>
        <themekey>Bethlehem Granodiorite</themekey>
        <themekey>Gile Mountain Formation</themekey>
        <themekey>Waits River Formation</themekey>
        <themekey>Littleton Formation</themekey>
        <themekey>Lake Memphremagog Intrusive Suite</themekey>
        <themekey>Comerford Intrusive Complex</themekey>
        <themekey>Fitch Formation</themekey>
        <themekey>Clough Quartzite</themekey>
        <themekey>Rangeley Formation</themekey>
        <themekey>Partridge Formation</themekey>
        <themekey>Ammonoosuc Volcanics</themekey>
        <themekey>Oliverian Plutonic Suite</themekey>
      </theme>
      <theme>
        <themekt>Lithologic classification of geologic map units</themekt>
        <themekey>Sedimentary rock</themekey>
        <themekey>Conglomerate</themekey>
        <themekey>Carbonate rock</themekey>
        <themekey>Limestone</themekey>
        <themekey>Mixed volcanic/clastic rock</themekey>
        <themekey>Felsic volcanic rock</themekey>
        <themekey>Dacite</themekey>
        <themekey>Intermediate volcanic rock</themekey>
        <themekey>Andesite</themekey>
        <themekey>Plutonic rock</themekey>
        <themekey>Lamprophyre</themekey>
        <themekey>Pegmatite</themekey>
        <themekey>Granitoid</themekey>
        <themekey>Granite</themekey>
        <themekey>Quartz diorite</themekey>
        <themekey>Diorite</themekey>
        <themekey>Diabase</themekey>
        <themekey>Granodiorite</themekey>
        <themekey>Trondhjemite</themekey>
        <themekey>Metamorphic rock</themekey>
        <themekey>Metasedimentary rock</themekey>
        <themekey>Slate</themekey>
        <themekey>Quartzite</themekey>
        <themekey>Metaconglomerate</themekey>
        <themekey>Marble</themekey>
        <themekey>Metavolcanic rock</themekey>
        <themekey>Greenstone</themekey>
        <themekey>Phyllite</themekey>
        <themekey>Schist</themekey>
        <themekey>Pelitic schist</themekey>
        <themekey>Amphibole schist</themekey>
        <themekey>Granofels</themekey>
        <themekey>Gneiss</themekey>
        <themekey>Migmatite</themekey>
        <themekey>Amphibolite</themekey>
        <themekey>Tectonic breccia</themekey>
        <themekey>Phyllonite</themekey>
      </theme>
      <theme>
        <themekt>USGS Metadata Identifier</themekt>
        <themekey>USGS:65c62f4ed34ef4b119cb27f4</themekey>
      </theme>
      <place>
        <placekt>Common geographic areas</placekt>
        <placekey>United States</placekey>
        <placekey>Vermont</placekey>
        <placekey>Windham County</placekey>
        <placekey>Windsor County</placekey>
        <placekey>Bellows Falls</placekey>
        <placekey>New Hampshire</placekey>
        <placekey>Cheshire</placekey>
        <placekey>Sullivan</placekey>
        <placekey>Alstead</placekey>
      </place>
    </keywords>
    <accconst>None. Acknowledgment of the U.S. Geological Survey would be appreciated in products derived from these data.</accconst>
    <useconst>None. Acknowledgment of the U.S. Geological Survey would be appreciated in products derived from these data. Although software enables the user to display images at various scales, map data in this report should not be used at scales larger than 1:24,000.</useconst>
    <ptcontac>
      <cntinfo>
        <cntorgp>
          <cntorg>U.S. Geological Survey, Northeast Region</cntorg>
          <cntper>Ernest A. Crider Jr.</cntper>
        </cntorgp>
        <cntpos>Geologist</cntpos>
        <cntaddr>
          <addrtype>mailing</addrtype>
          <address>Mail Stop 926A, 12201 Sunrise Valley Dr</address>
          <city>Reston</city>
          <state>VA</state>
          <postal>20192</postal>
          <country>US</country>
        </cntaddr>
        <cntvoice>703-648-6906</cntvoice>
        <cntfax>703-648-6953</cntfax>
        <cntemail>ecrider@usgs.gov</cntemail>
      </cntinfo>
    </ptcontac>
    <datacred>Funding for this report was provided by the National Cooperative Geologic Mapping Program (NCGMP) from 1994 to 2025. Prepared in cooperation with the State of Vermont, Vermont Agency of Natural Resources, Vermont Geological Survey; State of New Hampshire, Department of Environmental Services, New Hampshire Geological Survey</datacred>
    <native>Version 6.2 (Build 9200) ; Esri ArcGIS 10.6.0.8321</native>
  </idinfo>
  <dataqual>
    <attracc>
      <attraccr>Geologic contacts and information were garnered from 1:24,000-scale mapping of geologic material based on observation from fieldwork, previously published geologic maps, and unpublished geologic data in the region. The geologic information might change if additional outcrops are discovered or exposed as the natural land changes, or as the result of development, or advances in scientific research are made. The features in the database are not based on legal parcels or definitions.
Confidence that a feature exists and confidence that a feature is correctly identified are described in per-feature attributes ExistenceConfidence and IdentityConfidence.</attraccr>
    </attracc>
    <logic>Geologic contacts and information were garnered from 1:24,000-scale mapping of bedrock material based on observation from geologic fieldwork in the region. The geologic information might change if additional outcrops are discovered or exposed as the natural land changes or as the result of development. The features in the database are not based on legal parcels or definitions. Topology tests were performed to ensure the integrity of the data. These tests checked for polygon overlaps and gaps and line pseudos, dangles, and intersections. Additional tests were conducted to ensure that linework from geologic contacts match polygon boundaries where necessary.</logic>
    <complete>Dataset is considered complete for the information presented, as described in the abstract. Users are advised to read the rest of the metadata record carefully for additional details.</complete>
    <posacc>
      <horizpa>
        <horizpar>Data were delineated on classic U.S. Geological Survey (USGS) 7.5-minute topographic maps at 1:24,000 scale. Therefore, the horizontal accuracy is assumed to be within National Map Accuracy Standards, with a horizontal accuracy of 45.6 feet at the 95% confidence level. In addition, the horizontal accuracy standard requires that the positions of 90 percent of all points tested must be accurate within 1/50th of an inch (0.05 centimeters) on the map. For more information see U.S. Geological Survey Fact Sheet 171-99.
Estimated accuracy of horizontal location is given on a per-feature basis by attribute LocationConfidenceMeters. Values are expected to be correct within a factor of 2. A LocationConfidenceMeters value of -9 or -9999 indicates that no value has been assigned.</horizpar>
      </horizpa>
      <vertacc>
        <vertaccr>The data were delineated on classic U.S. Geological Survey (USGS) 7.5-minute topographic maps at 1:24,000 scale. Therefore, the vertical accuracy is assumed to be within National Map Accuracy Standards, with a vertical accuracy of 11.9 feet at the 95% confidence level. In addition, the vertical accuracy standard requires that the elevation of 90 percent of all points tested much be correct within half of the contour interval. For more information see U.S. Geological Survey Fact Sheet 171-99.</vertaccr>
      </vertacc>
    </posacc>
    <lineage>
      <srcinfo>
        <srccite>
          <citeinfo>
            <origin>Federal Geographic Data Committee (FGDC)</origin>
            <pubdate>2006</pubdate>
            <title>FGDC Digital Cartographic Standard for Geologic Map Symbolization</title>
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              <pubplace>Reston, VA</pubplace>
              <publish>U.S. Geological Survey</publish>
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            <othercit>Federal Geographic Data Committee [prepared for the Federal Geographic Data Committee by the U.S. Geological Survey], 2006, FGDC Digital Cartographic Standard for Geologic Map Symbolization: Reston, Va., Federal Geographic Data Committee Document Number FGDC-STD-013-2006, 290 p., 2 plates.</othercit>
            <onlink>https://ngmdb.usgs.gov/fgdc_gds/geolsymstd.php</onlink>
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        <typesrc>Digital and/or Hardcopy</typesrc>
        <srctime>
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          <srccurr>publication date</srccurr>
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        <srccitea>FGDC</srccitea>
        <srccontr>This citation was used in the production of this database, either in the description of map units, or the production of geologic polygons, contacts and faults, or the additional supporting structural and cartographic information.</srccontr>
      </srcinfo>
      <srcinfo>
        <srccite>
          <citeinfo>
            <origin>National Cooperative Geologic Mapping Program (NCGMP)</origin>
            <pubdate>2020</pubdate>
            <title>GeMS (Geologic Map Schema)—A standard format for the digital publication of geologic maps</title>
            <geoform>publication</geoform>
            <serinfo>
              <sername>Techniques and Methods</sername>
              <issue>book 11. chap. B10</issue>
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              <pubplace>Reston, VA</pubplace>
              <publish>U.S. Geological Survey</publish>
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            <othercit>U.S. Geological Survey National Cooperative Geologic Mapping Program, 2020, GeMS (Geologic Map Schema)—A standard format for the digital publication of geologic maps: U.S. Geological Survey Techniques and Methods, book 11. chap. B10, 74 p.</othercit>
            <onlink>https://doi.org/10.3133/tm11B10</onlink>
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        <srccitea>GeMS</srccitea>
        <srccontr>This citation was used in the production of this database, either in the description of map units, or the production of geologic polygons, contacts and faults, or the additional supporting structural and cartographic information.</srccontr>
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      <srcinfo>
        <srccite>
          <citeinfo>
            <origin>U.S. Geological Survey</origin>
            <origin>Science Publishing Network (SPN)</origin>
            <pubdate>2015</pubdate>
            <title>U.S. Geological Survey Science Publishing Network, MapStyleGuide_DMU_print_1sht_v1-1_01-15.pdf.</title>
            <geoform>publication</geoform>
            <othercit>U.S. Geological Survey Science Publishing Network, MapStyleGuide_DMU_print_1sht_v1-1_01-15.pdf.</othercit>
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        <srccitea>USGS</srccitea>
        <srccontr>This citation was used in the production of this database, either in the description of map units, or the production of geologic polygons, contacts and faults, or the additional supporting structural and cartographic information.</srccontr>
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      <srcinfo>
        <srccite>
          <citeinfo>
            <origin>K.K.E. Neuendorf</origin>
            <origin>J.P. Mehl, Jr</origin>
            <origin>J.A. Jackson</origin>
            <pubdate>2011</pubdate>
            <title>Glossary of geology</title>
            <edition>5</edition>
            <geoform>publication</geoform>
            <pubinfo>
              <pubplace>Alexandria, VA</pubplace>
              <publish>American Geosciences Institute</publish>
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            <othercit>Neuendorf, K.K.E., Mehl, J.P., Jr., and Jackson, J.A., eds., 2011, Glossary of geology (5th ed., revised): Alexandria, Va., American Geosciences Institute, 783 p.</othercit>
            <onlink>https://glossary.agi.org</onlink>
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          <srccurr>publication date</srccurr>
        </srctime>
        <srccitea>AGI</srccitea>
        <srccontr>This citation was used in the production of this database, either in the description of map units, or the production of geologic polygons, contacts and faults, or the additional supporting structural and cartographic information.</srccontr>
      </srcinfo>
      <srcinfo>
        <srccite>
          <citeinfo>
            <origin>A.J. Merschat</origin>
            <origin>G.J. Walsh</origin>
            <origin>P.M. Valley</origin>
            <origin>R.J. McAleer</origin>
            <origin>T.R. Armstrong</origin>
            <pubdate>20250526</pubdate>
            <title>Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire</title>
            <geoform>publication</geoform>
            <serinfo>
              <sername>Scientific Investigations Map</sername>
              <issue>3535</issue>
            </serinfo>
            <pubinfo>
              <pubplace>Reston, VA</pubplace>
              <publish>U.S. Geological Survey</publish>
            </pubinfo>
            <othercit>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</othercit>
            <onlink>https://doi.org/10.3133/sim3535</onlink>
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              <caldate>20250526</caldate>
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        <srccontr>This citation was used in the production of this database, either in the description of map units, or the production of geologic polygons, contacts and faults, or the additional supporting structural and cartographic information.</srccontr>
      </srcinfo>
      <srcinfo>
        <srccite>
          <citeinfo>
            <origin>C.K. McWilliams</origin>
            <origin>M.J. Kunk</origin>
            <origin>R.P. Wintsch</origin>
            <origin>D L. Bish</origin>
            <pubdate>20140127</pubdate>
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            <onlink>https://doi.org/10.1016/j.chemgeo.2005.03.011</onlink>
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        </srccite>
        <typesrc>Digital and/or Hardcopy</typesrc>
        <srctime>
          <timeinfo>
            <sngdate>
              <caldate>200507</caldate>
            </sngdate>
          </timeinfo>
          <srccurr>publication date</srccurr>
        </srctime>
        <srccitea>BF24KNHVTDAS17</srccitea>
        <srccontr>This citation was used in the production of this database, either in the description of map units, or the production of geologic polygons, contacts and faults, or the additional supporting structural and cartographic information.</srccontr>
      </srcinfo>
      <procstep>
        <procdesc>Base-map separate raster scans of 1,200 dots per square inch (dpi) of the 1:24,000-scale Bellows Falls 7.5- x 15-minute quadrangle were acquired from the U.S. Geological Survey Science Information Services in Rolla, Missouri. The scans were cleaned of scratches in Adobe Photoshop and registered in ArcGIS 10.5 as North American Datum of 1927, using Universal Transverse Mercator Projection, zone 18 north. Later, the base-map separations and base-map shapefiles were projected into North American Datum of 1983, New Hampshire State Plane coordinate system at the request of the authors. A vector water-layer (shapefile) was created using ArcGIS ArcScan to auto vectorize the water fill from the blue separate for use in creating concealed contacts, faults, and axial planes in the database.</procdesc>
        <procdate>20200402</procdate>
        <proccont>
          <cntinfo>
            <cntorgp>
              <cntorg>U.S. Geological Survey, Northeast Region</cntorg>
              <cntper>Ernest A Crider</cntper>
            </cntorgp>
            <cntpos>Geologist</cntpos>
            <cntaddr>
              <addrtype>mailing</addrtype>
              <address>Mail Stop 926A, 12201 Sunrise Valley Dr</address>
              <city>Reston</city>
              <state>VA</state>
              <postal>20192</postal>
              <country>US</country>
            </cntaddr>
            <cntvoice>703-648-6906</cntvoice>
            <cntfax>703-648-6953</cntfax>
            <cntemail>ecrider@usgs.gov</cntemail>
          </cntinfo>
        </proccont>
      </procstep>
      <procstep>
        <procdesc>A geodatabase was created using the GeMS database schema. Information (points, lines, and polygon data) from the author was obtained from a non-compliant geodatabase along with a scientifically reviewed Adobe Illustrator file with colors and additional information not included in the database. The GeMS compliant database schema was expanded to include information from the original database that is not in the GeMS schema. These include, but are not limited to, the Throughgoing, Parting, Fracture, Rotation, Width, Mineral1, and Mineral2 fields in the OrientationPoints feature class. For information about these additional fields, users are encouraged to read the metadata carefully. Individual feature classes were then loaded into the GeMS compliant database, and fields from the original dataset were matched into the GeMS compliant database. The original ContactsandFaults layer was carefully smoothed (with the advanced editing toolbar) and the associated MapUnitPolys were recreated using those smoothed lines. The symbol field was populated with the appropriate numbers from the Federal Geographic Data Committee (FGDC) CMYK color chart (https://ngmdb.usgs.gov/fgdcgds/geolsymstd/download.php) approximating (and in some case adjusting) the colors used in the Adobe Illustrator map produced by the author. The Type field in the ContactsandFaults and GeologicLines layers were adjusted to fit the explanation of map symbols on the published map. The ContactsandFaults and GeologicLines feature classes were then symbolized using ArcGIS representation classes and the MapUnitPolys layer was matched to the USGSsymbols.style file for color reproduction. Following this, the OrientationPoints and OverlayPolys feature classes were loaded into the dataset.</procdesc>
        <procdate>20200402</procdate>
      </procstep>
      <procstep>
        <procdesc>Representation classes were then applied to the OrientationPoint feature class. Some of the symbols were customized or repurposed for the published geologic map and the dataset. The OrientationPoints were then adjusted to ensure they were inside existing OverlayPolys (Outcrops), pulled apart where overlapping symbols existed, or hidden (made not visible) where structural measurements were overwhelming. Some information from the OrientationPoints feature class was removed and placed into the GenericPoints feature class, these included mines, spring, and some stations.</procdesc>
        <procdate>20200402</procdate>
      </procstep>
      <procstep>
        <procdesc>Once edited, the Type field in the OrientationPoints feature class was adjusted to match the Explanation of Map symbols on the published geologic map. Labels on the published geologic map were created using Annotation feature classes. The dataset was then exported to Adobe Illustrator to produce the published geologic map.</procdesc>
        <procdate>20240804</procdate>
      </procstep>
      <procstep>
        <procdesc>Following the deprecation of cartographic representation in ArcPro during the editing process; cartography was completed using the .styleX format in ArcGIS Pro using a custom stylesheet and a unique SymbolX field, exclusive to the OrientationPoints feature class. Annotation features classes were deleted since the U.S. Geological Survey science publishing network did not properly use them in preparation for the paper geologic map. PlotAtScale was used, where necessary in order to hide structural measurements where they were overwhelming.</procdesc>
        <procdate>20241201</procdate>
        <proccont>
          <cntinfo>
            <cntorgp>
              <cntorg>U.S. Geological Survey, Northeast Region</cntorg>
              <cntper>Ernest A Crider</cntper>
            </cntorgp>
            <cntpos>Geologist</cntpos>
            <cntaddr>
              <addrtype>mailing address</addrtype>
              <address>Mail Stop 926A, 12201 Sunrise Valley Dr</address>
              <city>Reston</city>
              <state>VA</state>
              <postal>20192</postal>
              <country>US</country>
            </cntaddr>
            <cntvoice>703-648-6906</cntvoice>
            <cntfax>703-648-6953</cntfax>
            <cntemail>ecrider@usgs.gov</cntemail>
          </cntinfo>
        </proccont>
      </procstep>
      <procstep>
        <procdesc>After editing, information from the edited map was placed into the DataSources, DescriptionofMapUnits, and Glossary object classes. Annotation features classes were forcefully redone since the U.S. Geological Survey science publishing network did not properly use them in the preparation of the published geologic map.  Additional attributes to edit and complete the GeMS database schema were added at this time including information about LocationConfidenceMeters, ExistenceConfidence, and IdentityConfidence.</procdesc>
        <procdate>20250513</procdate>
      </procstep>
    </lineage>
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  <spdoinfo>
    <direct>Vector</direct>
    <ptvctinf>
      <sdtsterm>
        <sdtstype>G-polygon</sdtstype>
        <ptvctcnt>12,326</ptvctcnt>
      </sdtsterm>
    </ptvctinf>
  </spdoinfo>
  <spref>
    <horizsys>
      <planar>
        <mapproj>
          <mapprojn>Transverse_Mercator</mapprojn>
          <mapprojp>
            <feast>984250.0</feast>
            <fnorth>0.0</fnorth>
            <latprjo>0.0</latprjo>
            <longcm>-71.6666666666667</longcm>
            <stdparll>0.0</stdparll>
            <stdparll>0.0</stdparll>
          </mapprojp>
        </mapproj>
        <planci>
          <plance>coordinate pair</plance>
          <coordrep>
            <absres>0.6096</absres>
            <ordres>0.6096</ordres>
          </coordrep>
          <plandu>meters</plandu>
        </planci>
      </planar>
      <geodetic>
        <horizdn>North_American_Datum_1983</horizdn>
        <ellips>GRS 1980</ellips>
        <semiaxis>6378137.0</semiaxis>
        <denflat>298.257222101</denflat>
      </geodetic>
    </horizsys>
  </spref>
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        <enttypl>DescriptionOfMapUnits</enttypl>
        <enttypd>Non-spatial table that captures content of the Description of Map Units (or equivalent List of Map Units and associated pamphlet text) included in a traditional paper geologic map. Has an internal hierarchy expressed by attribute HierarchyKey</enttypd>
        <enttypds>GeMS</enttypds>
      </enttyp>
      <attr>
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        <attrdef>Internal feature number</attrdef>
        <attrdefs>ESRI</attrdefs>
        <attrdomv>
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      <attr>
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            <edomv>DSwvf</edomv>
            <edomvd>Felsic volcanic member of the Waits River Formation</edomvd>
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            <edomvd>Metafelsite volcanics and granofels member of the Partridge Formation</edomvd>
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          <edom>
            <edomv>Dgqs</edomv>
            <edomvd>Gray quartzite and metapelite member of the Gile Mountain Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
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        <attrdomv>
          <edom>
            <edomv>Ops</edomv>
            <edomvd>Pelitic schist and granofels member of the Partridge Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
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        <attrdomv>
          <edom>
            <edomv>Srps</edomv>
            <edomvd>Porphyroblastic sillimanite schist member of the Rangeley Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
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        <attrdomv>
          <edom>
            <edomv>DSwsv</edomv>
            <edomvd>Metavolcaniclastic members of the Waits River Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
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          <edom>
            <edomv>Kd</edomv>
            <edomvd>Mafic dikes of the White Mountain Igneous Suite</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
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        <attrdomv>
          <edom>
            <edomv>Dbg</edomv>
            <edomvd>Bethlehem Granodiorite of the New Hampshire Plutonic Suite</edomvd>
            <edomvds>BF24KNHVTDAS03 | BF24KNHVTDAS07 | BF24KNHVTDAS08</edomvds>
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        <attrdomv>
          <edom>
            <edomv>Sf</edomv>
            <edomvd>Fitch Formation</edomvd>
            <edomvds>BF24KNHVTDAS12 | BF24KNHVTDAS08</edomvds>
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        <attrdomv>
          <edom>
            <edomv>DSwv</edomv>
            <edomvd>Laminated schist and granofels member of the Waits River Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
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        <attrdomv>
          <edom>
            <edomv>Oog</edomv>
            <edomvd>Granite gneiss of the Alstead dome</edomvd>
            <edomvds>BF24KNHVTDAS04 | BF24KNHVTDAS15</edomvds>
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        <attrdomv>
          <edom>
            <edomv>Dg</edomv>
            <edomvd>Granite dikes of the New Hampshire Plutonic Suite</edomvd>
            <edomvds>Ratcliffe, N.M., Stanley, R.S., Gale, M.H., Thompson, P.J., and Walsh, G.J., 2011, Bedrock geologic map of Vermont: U.S. Geological Survey Scientific Investigations Map 3184, 3 sheets, scale 1:100,000.</edomvds>
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        <attrdomv>
          <edom>
            <edomv>Srq</edomv>
            <edomvd>Quartzite, calc-silicate, and schist member of the Rangeley Formation</edomvd>
            <edomvds>BF24KNHVTDAS14 | BF24KNHVTDAS07</edomvds>
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        <attrdomv>
          <edom>
            <edomv>Scd</edomv>
            <edomvd>Metadiabase dikes of the Comerford Intrusive Complex</edomvd>
            <edomvds>Rankin, D.W., Coish, R.A., Tucker, R.D., Peng, Z.X., Wilson, S.A., and Rouff, A.A., 2007, Silurian extension in the upper Connecticut Valley, United States, and the origin of middle Paleozoic basins in the Québec embayment: American Journal of Science, v. 307, no. 1, p. 216–264.</edomvds>
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        <attrdomv>
          <edom>
            <edomv>Dl</edomv>
            <edomvd>Littleton Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
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        <attrdomv>
          <edom>
            <edomv>Sca</edomv>
            <edomvd>Amphibolite member of the Clough Quartzite</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
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        <attrdomv>
          <edom>
            <edomv>Mzsz</edomv>
            <edomvd>Breccia or silicified zone</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
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        <attrdomv>
          <edom>
            <edomv>DSwhg</edomv>
            <edomvd>Hornblende-plagioclase gneiss member of the Waits River Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
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        <attrdomv>
          <edom>
            <edomv>Dbd</edomv>
            <edomvd>Bethlehem quartz diorite of the New Hampshire Plutonic Suite</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
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        <attrdomv>
          <edom>
            <edomv>Oaf</edomv>
            <edomvd>Intermediate to felsic metatuff member of the Ammonoosuc Volcanics</edomvd>
            <edomvds>BF24KNHVTDAS03 | BF24KNHVTDAS15</edomvds>
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        <attrdomv>
          <edom>
            <edomv>Scs</edomv>
            <edomvd>Muscovite schist member of the Clough Quartzite</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
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        <attrdomv>
          <edom>
            <edomv>DSws</edomv>
            <edomvd>Gray phyllite and schist member of the Waits River Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
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        <attrdomv>
          <edom>
            <edomv>Op</edomv>
            <edomvd>Rusty schist and granofels member of the Partridge Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
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        <attrdomv>
          <edom>
            <edomv>DSwa</edomv>
            <edomvd>Amphibolite and greenstone member of the Waits River Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
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        <attrdomv>
          <edom>
            <edomv>DSwr</edomv>
            <edomvd>Rusty schist member of the Waits River Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
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        <attrdomv>
          <edom>
            <edomv>Oot</edomv>
            <edomvd>Trondhjemite gneiss of the Alstead dome</edomvd>
            <edomvds>BF24KNHVTDAS03 | BF24KNHVTDAS15</edomvds>
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        <attrdomv>
          <edom>
            <edomv>Dgq</edomv>
            <edomvd>Feldspathic quartzite, granofels, and metapelite member of the Gile Mountain Formation</edomvd>
            <edomvds>Walsh, G.J., Valley, P.M., Armstrong, T.R., Ratcliffe, N.M., Merschat, A.J., and Gentry, B.J., 2020, Bedrock geologic map of the Springfield 7.5- x 15-minute quadrangle, Windsor County, Vermont, and Sullivan County, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3462, 2 sheets, scale 1:24,000.</edomvds>
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        <attrdomv>
          <edom>
            <edomv>Sfc</edomv>
            <edomvd>Metaconglomerate member of the Fitch Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
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        <attrdomv>
          <edom>
            <edomv>MDp</edomv>
            <edomvd>Muscovite-biotite pegmatite of the New Hampshire Plutonic suite</edomvd>
            <edomvds>Bradley, D.C., Shea, E., Buchwaldt, R., Bowring, S., Benowitz, J., O’Sullivan, P., and McCauley, A., 2016, Geochronology and tectonic context of lithium-cesium-tantalum pegmatites in the Appalachians: Canadian Mineralogist, v. 54, no. 4, p. 945–969.</edomvds>
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        <attrdomv>
          <edom>
            <edomv>Sr</edomv>
            <edomvd>Schist and granofels member of the Rangeley Formation</edomvd>
            <edomvds>BF24KNHVTDAS14 | BF24KNHVTDAS07</edomvds>
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        <attrdomv>
          <edom>
            <edomv>PSph</edomv>
            <edomvd>Phyllonite, undivided</edomvd>
            <edomvds>BF24KNHVTDAS02 | BF24KNHVTDAS03 | BF24KNHVTDAS04</edomvds>
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        <attrdomv>
          <edom>
            <edomv>DSwl</edomv>
            <edomvd>Limestone and schist member of the Waits River Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
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        <attrdomv>
          <edom>
            <edomv>Scq</edomv>
            <edomvd>Quartzite and metaconglomerate member of the Clough Quartzite</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
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        <attrdomv>
          <edom>
            <edomv>Opa</edomv>
            <edomvd>Amphibolite member of the Partridge Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
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        <attrdomv>
          <edom>
            <edomv>Src</edomv>
            <edomvd>Metaconglomerate, granofels, and schist member of the Rangeley Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>DSwqc</edomv>
            <edomvd>Quartz-pebble to polymict conglomerate member of the Waits River Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>DSwvq</edomv>
            <edomvd>Metavolcaniclastic members of the Waits River Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>DSwg</edomv>
            <edomvd>Large-garnet and hornblende garbenscheifer schist member of the Waits River Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Oaa</edomv>
            <edomvd>Amphibolite member of the Ammonoosuc Volcanics</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Name</attrlabl>
        <attrdef>Name of map unit, as shown in boldface in traditional DMU, e.g., "Shnabkaib Member". Identifies unit within its hierarchical context.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>FullName</attrlabl>
        <attrdef>Name of map unit including identification of containing higher rank unit(s), e.g., "Shnabkaib Member of Moenkopi Formation".</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Age</attrlabl>
        <attrdef>Age of map unit as shown in Description of Map Units. Examples of values are "late Holocene", "Pliocene and Miocene", "Lower Cretaceous".</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Description</attrlabl>
        <attrdef>Free-format text description of map unit. Commonly structured according to one or more accepted traditions (e.g., lithology, thickness, color, weathering and outcrop characteristics, distinguishing features, genesis, age constraints) and terse.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>HierarchyKey</attrlabl>
        <attrdef>String that records hierarchical structure. Has form nn-nn-nn, nnn-nnn, or similar. Numeric, left-padded with zeros, dash-delimited. Each HierarchyKey fragment of each row MUST be the same length to allow text-based sorting of table entries.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>ParagraphStyle</attrlabl>
        <attrdef>Token that identifies formatting of paragraph(s) within traditional Description of Map Units that correspond to this table entry.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <edom>
            <edomv>DMU Unit 1</edomv>
            <edomvd>Times New Roman, Bold, 10 pt, 12 pt leading, all caps, centered, 12 pt space before</edomvd>
            <edomvds>U.S. Geological Survey Science Publishing Network, MapStyleGuide_DMU_print_1sht_v1-1_01-15.pdf.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>DMU Heading 3</edomv>
            <edomvd>Times New Roman, Bold, 10 pt, 12 pt leading, all caps, centered, 12 pt space before</edomvd>
            <edomvds>U.S. Geological Survey Science Publishing Network, MapStyleGuide_DMU_print_1sht_v1-1_01-15.pdf.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>DMU Bracketed Headnote - 1 Line</edomv>
            <edomvd>Times New Roman, Regular, 10 pt, 12 pt leading, centered, 8 pt space before</edomvd>
            <edomvds>U.S. Geological Survey Science Publishing Network, MapStyleGuide_DMU_print_1sht_v1-1_01-15.pdf.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>DMU Heading 1 (DMU Title)</edomv>
            <edomvd>Times New Roman, Bold, 12 pt, 12 pt leading, all caps, centered</edomvd>
            <edomvds>U.S. Geological Survey Science Publishing Network, MapStyleGuide_DMU_print_1sht_v1-1_01-15.pdf.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>DMU Heading 2</edomv>
            <edomvd>Times New Roman, Bold, 10 pt, 12 pt leading, all caps, centered, 12 pt space before</edomvd>
            <edomvds>U.S. Geological Survey Science Publishing Network, MapStyleGuide_DMU_print_1sht_v1-1_01-15.pdf.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>DMU Unit 1 w/box (no space between box above)</edomv>
            <edomvd>Times New Roman, Regular, 10 pt, 12 pt leading, left justified, 66 pt left indent, –20 pt 1st line indent, 6 pt space 
before</edomvd>
            <edomvds>U.S. Geological Survey Science Publishing Network, MapStyleGuide_DMU_print_1sht_v1-1_01-15.pdf.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>DMU Heading 4</edomv>
            <edomvd>Times New Roman, Bold, 10 pt, 12 pt leading, all caps, centered, 12 pt space before</edomvd>
            <edomvds>U.S. Geological Survey Science Publishing Network, MapStyleGuide_DMU_print_1sht_v1-1_01-15.pdf.</edomvds>
          </edom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Label</attrlabl>
        <attrdef>Plain-text equivalent of the desired annotation for a feature: for example "14 Ma", or "^c" which (when used with the FGDC GeoAge font) results in the geologic map-unit label TRc (with TR run together to make the Triassic symbol).</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Symbol</attrlabl>
        <attrdef>Reference to a point marker, line symbol, or area-fill symbol that is used on the map graphic to denote the feature: perhaps a star for a K-Ar age locality, or a heavy black line for a fault.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>AreaFillRGB</attrlabl>
        <attrdef>{Red, Green, Blue} tuples that specify the suggested color (e.g., "255,255,255", "124,005,255") of area fill for symbolizing MapUnit. Each color value is an integer between 0 and 255, values are zero-padded to a length of 3 digits, and values are separated by commas with no space: NNN,NNN,NNN.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>AreaFillPatternDescription</attrlabl>
        <attrdef>Text description (e.g., "random small red dashes") provided as a convenience for users who must recreate symbolization.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>DescriptionSourceID</attrlabl>
        <attrdef>Source of map-unit description; foreign key to table Datasources.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <edom>
            <edomv>BF24KNHVTDAS08</edomv>
            <edomvd>Walsh, G.J., Valley, P.M., Armstrong, T.R., Ratcliffe, N.M., Merschat, A.J., and Gentry, B.J., 2020, Bedrock geologic map of the Springfield 7.5- x 15-minute quadrangle, Windsor County, Vermont, and Sullivan County, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3462, 2 sheets, scale 1:24,000.</edomvd>
            <edomvds>This report</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>BF24KNHVTDAS06</edomv>
            <edomvd>Ratcliffe, N.M., Stanley, R.S., Gale, M.H., Thompson, P.J., and Walsh, G.J., 2011, Bedrock geologic map of Vermont: U.S. Geological Survey Scientific Investigations Map 3184, 3 sheets, scale 1:100,000.</edomvd>
            <edomvds>This report</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>BF24KNHVTDAS03 | BF24KNHVTDAS07 | BF24KNHVTDAS08</edomv>
            <edomvd>BF24KNHVTDAS03 | BF24KNHVTDAS07 | BF24KNHVTDAS08</edomvd>
            <edomvds>This report</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>BF24KNHVTDAS09 | BF24KNHVTDAS10</edomv>
            <edomvd>BF24KNHVTDAS09 | BF24KNHVTDAS10</edomvd>
            <edomvds>This report</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>BF24KNHVTDAS11</edomv>
            <edomvd>Rankin, D.W., Coish, R.A., Tucker, R.D., Peng, Z.X., Wilson, S.A., and Rouff, A.A., 2007, Silurian extension in the upper Connecticut Valley, United States, and the origin of middle Paleozoic basins in the Québec embayment: American Journal of Science, v. 307, no. 1, p. 216–264.</edomvd>
            <edomvds>This report</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>BF24KNHVTDAS03 | BF24KNHVTDAS15</edomv>
            <edomvd>BF24KNHVTDAS03 | BF24KNHVTDAS15</edomvd>
            <edomvds>This report</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>BF24KNHVTDAS04 | BF24KNHVTDAS15</edomv>
            <edomvd>BF24KNHVTDAS04 | BF24KNHVTDAS15</edomvd>
            <edomvds>This report</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>BF24KNHVTDAS01</edomv>
            <edomvd>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvd>
            <edomvds>This report</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>BF24KNHVTDAS14 | BF24KNHVTDAS07</edomv>
            <edomvd>BF24KNHVTDAS14 | BF24KNHVTDAS07</edomvd>
            <edomvds>This report</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>BF24KNHVTDAS13</edomv>
            <edomvd>Walsh, G.J., 2016, Bedrock geologic map of the Hartland and North Hartland quadrangles, Windsor County, Vermont, and Sullivan and Grafton Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3361, 2 sheets, scale 1:24,000.</edomvd>
            <edomvds>This report</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>BF24KNHVTDAS12 | BF24KNHVTDAS08</edomv>
            <edomvd>BF24KNHVTDAS12 | BF24KNHVTDAS08</edomvd>
            <edomvds>This report</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>BF24KNHVTDAS02 | BF24KNHVTDAS03 | BF24KNHVTDAS04</edomv>
            <edomvd>BF24KNHVTDAS02 | BF24KNHVTDAS03 | BF24KNHVTDAS04</edomvd>
            <edomvds>This report</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>BF24KNHVTDAS05</edomv>
            <edomvd>Bradley, D.C., Shea, E., Buchwaldt, R., Bowring, S., Benowitz, J., O’Sullivan, P., and McCauley, A., 2016, Geochronology and tectonic context of lithium-cesium-tantalum pegmatites in the Appalachians: Canadian Mineralogist, v. 54, no. 4, p. 945–969.</edomvd>
            <edomvds>This report</edomvds>
          </edom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>GeoMaterial</attrlabl>
        <attrdef>Categorization of map unit based on lithologic and genetic character, term selected from NGMDB standard term list defined in Appendix A of GeMS documentation, available at http://ngmdb.usgs.gov/Info/standards/GeMS..</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <edom>
            <edomv>Deformation-related metamorphic rock</edomv>
            <edomvd>Rock derived from preexisting rocks by essentially solid-state mineralogical, chemical, or structural changes in response to strong deformation, commonly in association with marked changes in temperature, pressure, and (or) chemical environment. Generally forms in narrow, planar zones of local deformation (for example, along faults); characterized by foliation or alignment of mineral grains. Includes mylonite and cataclasite.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Conglomerate</edomv>
            <edomvd>Sedimentary rock, composed predominantly of particles or clasts derived by erosion and weathering of preexisting rock; contains more than 30 percent gravel-sized clasts.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Coarse-grained, felsic-composition intrusive igneous rock</edomv>
            <edomvd>Rock that solidified from molten or partly molten material (magma) at some depth beneath Earths surface, thereby cooling slowly enough for mineral crystals to grow large enough to be visible to naked eye. Composed mostly of light-colored minerals (for example, feldspar, quartz). Includes granitic, syenitic, and monzonitic rock.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Meta-felsic and intermediate rock</edomv>
            <edomvd>Rock derived from preexisting felsic and intermediate-composition rocks by essentially solid-state, mineralogical, chemical, or structural changes, in response to marked changes in temperature, pressure, deformation, and (or) chemical environment, generally at depth in Earths crust. Composed mostly of light-colored minerals; relatively enriched in silica. Includes metagranite, metadiorite, and meta-andesite.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Meta-mafic rock</edomv>
            <edomvd>Rock derived from preexisting mafic rocks by essentially solid-state, mineralogical, chemical, or structural changes, in response to marked changes in temperature, pressure, deformation, and (or) chemical environment, generally at depth in Earths crust. Composed mostly of iron- and magnesium-bearing, dark-colored and (or) green minerals. Includes greenstone, amphibolite, and metagabbro.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Coarse-grained, intermediate-composition intrusive igneous rock</edomv>
            <edomvd>Rock that solidified from molten or partly molten material (magma) at some depth beneath Earths surface, thereby cooling slowly enough for mineral crystals to grow large enough to be visible to naked eye. Intermediate in color and in mineral composition (between felsic and mafic igneous rock). Includes dioritic rock.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Medium and high-grade regional metamorphic rock, of unspecified origin</edomv>
            <edomvd>Rock derived from preexisting rocks and altered by essentially solid-state mineralogical, chemical, or structural changes, in response to relatively intense regional changes in temperature, pressure, deformation, and (or) chemical environment, generally at depth in Earths crust. Origin of preexisting rock is mixed (for example, igneous and sedimentary) or is not known. Includes amphibolite, granulite, schist, and gneiss.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Lower-grade metamorphic rock, of unspecified origin</edomv>
            <edomvd>Rock derived from preexisting rocks and altered by essentially solid-state mineralogical, chemical, or structural changes, in response to relatively mild regional changes in temperature, pressure, deformation, and (or) chemical environment, generally at depth in Earths crust. Origin of preexisting rock is mixed (for example, igneous and sedimentary) or is not known. Includes slate and phyllite.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Slate and phyllite, of sedimentary-rock origin</edomv>
            <edomvd>Fine-grained rock derived from preexisting sedimentary rocks and altered by essentially solid-state mineralogical, chemical, or structural changes, in response to marked changes in temperature, pressure, deformation, and (or) chemical environment, generally at depth in Earths crust. Includes phyllite and slate (compact, fine-grained rock that possesses strong cleavage and, hence, can be split into slabs and thin plates). Mostly formed from fine-grained material such as mudstone.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Fine-grained, felsic-composition intrusive igneous rock</edomv>
            <edomvd>Rock that solidified from molten or partly molten material (magma) at shallow depth beneath Earths surface, thereby cooling quickly. Generally fine grained but may contain large mineral crystals (phenocrysts). Mostly found as tabular dikes or sills. Composed mostly of light-colored minerals. Includes rhyolitic, dacitic, trachytic, and latitic rock.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Meta-volcaniclastic rock</edomv>
            <edomvd>Rock derived from preexisting volcaniclastic rocks by essentially solid-state, mineralogical, chemical, or structural changes, in response to marked changes in temperature, pressure, deformation, and (or) chemical environment, generally at depth in Earths crust. Composed of deformed but recognizable particles or clasts of volcanic explosive material.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Fine-grained, mafic-composition intrusive igneous rock</edomv>
            <edomvd>Rock that solidified from molten or partly molten material (magma) at shallow depth beneath Earths surface, thereby cooling quickly. Generally fine grained but may contain large mineral crystals (phenocrysts). Mostly found as tabular dikes or sills. Composed mostly of dark-colored minerals. Includes basaltic rock.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Schist and gneiss, of sedimentary-rock origin</edomv>
            <edomvd>Foliated rock derived from preexisting sedimentary rocks by essentially solid-state mineralogical, chemical, or structural changes in response to marked changes in temperature, pressure, deformation, and (or) chemical environment, generally at depth in Earths crust. Includes schist (characterized by such strong foliation or alignment of minerals that it readily splits into flakes or slabs) and gneiss (characterized by alternating, irregular bands of different mineral composition). Mostly formed from fine-grained material such as mudstone.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Quartzite</edomv>
            <edomvd>Rock derived from preexisting quartz-rich sedimentary rocks (commonly sandstone) and altered by essentially solid-state mineralogical, chemical, or structural changes, in response to marked changes in temperature, pressure, shear stress, and (or) chemical environment, generally at depth in Earths crust.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>GeoMaterialConfidence</attrlabl>
        <attrdef>Describes appropriateness of GeoMaterial term for describing the map unit.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <edom>
            <edomv>Medium</edomv>
            <edomvd>The term and definition generally characterize the overall lithology of the map unit, but there are one or more significant minor lithologies that are not adequately described by the selected term.</edomvd>
            <edomvds>GeMS documentation</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>High</edomv>
            <edomvd>The term and definition adequately characterize the overall lithologic nature of rocks and sediments in the map unit. Regarding the subjective term "adequately characterize", we refer to context and objectives of this classification as described in the GeMS documentation.</edomvd>
            <edomvds>GeMS documentation</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Low</edomv>
            <edomvd>The overall lithology of this map unit is not adequately classifiable using this list of terms and definitions, but the term selected is the best available.  Or this map unit is insufficiently known to confidently assign a GeoMaterial term.</edomvd>
            <edomvds>GeMS documentation</edomvds>
          </edom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>DescriptionOfMapUnits_ID</attrlabl>
        <attrdef>Primary key.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Arbitrary string. Values should be unique within this database.</udom>
        </attrdomv>
      </attr>
    </detailed>
    <detailed>
      <enttyp>
        <enttypl>DataSources</enttypl>
        <enttypd>Non-spatial table of sources of all spatial features, sources of some attributes of spatial features, and sources of some attributes of non-spatial table entries.</enttypd>
        <enttypds>GeMS</enttypds>
      </enttyp>
      <attr>
        <attrlabl>OBJECTID</attrlabl>
        <attrdef>Internal feature number</attrdef>
        <attrdefs>ESRI</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Source</attrlabl>
        <attrdef>Plain-text short description that identifies the data source.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Notes</attrlabl>
        <attrdef>Additional information specific to a particular feature or table entry.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain. Free text. Values of &lt;null&gt; or #null indicate no entry.</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>URL</attrlabl>
        <attrdef>Universal Resource Locator (URL) or Document Object Identifier (DOI), identifies a document on the World Wide Web.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>DataSources_ID</attrlabl>
        <attrdef>Primary key.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Arbitrary string. Values should be unique within this database.</udom>
        </attrdomv>
      </attr>
    </detailed>
    <detailed>
      <enttyp>
        <enttypl>Glossary</enttypl>
        <enttypd>Non-spatial table that, for certain fields (including all Type fields, Confidence fields, and GeneralLithology), lists the terms that populate these fields, term definitions, and sources for definitions.</enttypd>
        <enttypds>GeMS</enttypds>
      </enttyp>
      <attr>
        <attrlabl>OBJECTID</attrlabl>
        <attrdef>Internal feature number</attrdef>
        <attrdefs>ESRI</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Term</attrlabl>
        <attrdef>Plain-language word for a concept. Values must be unique within database as a whole.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Definition</attrlabl>
        <attrdef>Plain-language definition.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>DefinitionSourceID</attrlabl>
        <attrdef>Source of definition; foreign key to DataSources.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <edom>
            <edomv>GeMS</edomv>
            <edomvd>U.S. Geological Survey National Cooperative Geologic Mapping Program, 2020, GeMS (Geologic Map Schema)—A standard format for the digital publication of geologic maps: U.S. Geological Survey Techniques and Methods, book 11. chap. B10, 74 p.</edomvd>
            <edomvds>This report</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>FGDC</edomv>
            <edomvd>Federal Geographic Data Committee [prepared for the Federal Geographic Data Committee by the U.S. Geological Survey], 2006, FGDC Digital Cartographic Standard for Geologic Map Symbolization: Reston, Va., Federal Geographic Data Committee Document Number FGDC-STD-013-2006, 290 p., 2 plates.</edomvd>
            <edomvds>This report</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>AGI | BF24KNHVTDAS01</edomv>
            <edomvd>AGI | BF24KNHVTDAS01</edomvd>
            <edomvds>This report</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>BF24KNHVTDAS01</edomv>
            <edomvd>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvd>
            <edomvds>This report</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>BF24KNHVTDAS17</edomv>
            <edomvd>Mattinson, J.M., 2005, Zircon U-Pb chemical abrasion ("CA–TIMS") method: combined annealing and multi-step dissolution analysis for improved precision and accuracy of zircon ages: Chemical Geology, v. 220, p. 47–66.</edomvd>
            <edomvds>This report</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>USGS</edomv>
            <edomvd>U.S. Geological Survey Science Publishing Network, MapStyleGuide_DMU_print_1sht_v1-1_01-15.pdf.</edomvd>
            <edomvds>This report</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>AGI</edomv>
            <edomvd>Neuendorf, K.K.E., Mehl, J.P., Jr., and Jackson, J.A., eds., 2011, Glossary of geology (5th ed., revised): Alexandria, Va., American Geosciences Institute, 783 p.</edomvd>
            <edomvds>This report</edomvds>
          </edom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Glossary_ID</attrlabl>
        <attrdef>Primary key.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Arbitrary string. Values should be unique within this database.</udom>
        </attrdomv>
      </attr>
    </detailed>
    <detailed>
      <enttyp>
        <enttypl>GeoMaterialDict</enttypl>
        <enttypd>Non-spatial table that provides values of GeoMaterial, placed in a hierarchy, and their definitions. For further information, see Appendix A in GeMS documentation, available at http://ngmdb.usgs.gov/Info/standards/GeMS.</enttypd>
        <enttypds>GeMS</enttypds>
      </enttyp>
      <attr>
        <attrlabl>OBJECTID</attrlabl>
        <attrdef>Internal feature number</attrdef>
        <attrdefs>ESRI</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>HierarchyKey</attrlabl>
        <attrdef>String that records hierarchical structure. Has form nn-nn-nn, nnn-nnn, or similar. Numeric, left-padded with zeros, dash-delimited. Each HierarchyKey fragment of each row MUST be the same length to allow text-based sorting of table entries.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>GeoMaterial</attrlabl>
        <attrdef>Categorization of map unit based on lithologic and genetic character, term selected from NGMDB standard term list defined in Appendix A of GeMS documentation, available at http://ngmdb.usgs.gov/Info/standards/GeMS..</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <edom>
            <edomv>Volcanic mass flow</edomv>
            <edomvd>Volcanic deposits formed by mass movement (for example, debris avalanches, debris flows, lahar deposits), in many cases triggered by volcanic eruption. Debris avalanches that occur on volcanoes clearly without eruptive trigger may be classified as sedimentary (for example, as Debris flows, landslides, and other localized mass-movement sediment).</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Mass movement sediment</edomv>
            <edomvd>Sediment formed by downslope transport of particles or clasts produced by weathering and breakdown of underlying rock, sediment, and (or) soil. Composed of poorly sorted and poorly stratified material that ranges in size from clay to boulders. Includes colluvial, landslide, talus, and rock-avalanche deposits.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Marine sediment, mostly coarse-grained</edomv>
            <edomvd>Mud, sand, and gravel eroded from rocks and sediment on land, transported by streams, and deposited in marine deltas and basins. Mostly siliceous in composition.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Fine-grained, mafic-composition intrusive igneous rock</edomv>
            <edomvd>Rock that solidified from molten or partly molten material (magma) at shallow depth beneath Earths surface, thereby cooling quickly. Generally fine grained but may contain large mineral crystals (phenocrysts). Mostly found as tabular dikes or sills. Composed mostly of dark-colored minerals. Includes basaltic rock.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Lacustrine sediment, mostly fine-grained</edomv>
            <edomvd>Mostly well-sorted and well-bedded material, generally silt and clay sized, with lesser amounts of sand, deposited in perennial to intermittent lakes.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Marine sediment, mostly fine-grained</edomv>
            <edomvd>Mostly clay- and silt-sized sediment, deposited in relatively deep, quiet water, far removed from areas where coarser grained clastic sediments are washed into marine environment. Includes sediment derived from marine organisms.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Igneous rock</edomv>
            <edomvd>Rock and fragmental material that solidified from molten or partly molten material (magma).</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Intrusive igneous rock</edomv>
            <edomvd>Rock that solidified from molten or partly molten material (magma) below Earths surface.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Lacustrine sediment, mostly coarse-grained</edomv>
            <edomvd>Mostly well-sorted and well-bedded material, generally sand and gravel sized, with lesser amounts of silt and clay, deposited in perennial to intermittent lakes. Much of sediment is derived from material eroded and transported by streams. Mostly deposits of lake-marginal beaches and deltas.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Meta-felsic and intermediate rock</edomv>
            <edomvd>Rock derived from preexisting felsic and intermediate-composition rocks by essentially solid-state, mineralogical, chemical, or structural changes, in response to marked changes in temperature, pressure, deformation, and (or) chemical environment, generally at depth in Earths crust. Composed mostly of light-colored minerals; relatively enriched in silica. Includes metagranite, metadiorite, and meta-andesite.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Coarse-grained, intermediate-composition intrusive igneous rock</edomv>
            <edomvd>Rock that solidified from molten or partly molten material (magma) at some depth beneath Earths surface, thereby cooling slowly enough for mineral crystals to grow large enough to be visible to naked eye. Intermediate in color and in mineral composition (between felsic and mafic igneous rock). Includes dioritic rock.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Medium and high-grade regional metamorphic rock, of unspecified origin</edomv>
            <edomvd>Rock derived from preexisting rocks and altered by essentially solid-state mineralogical, chemical, or structural changes, in response to relatively intense regional changes in temperature, pressure, deformation, and (or) chemical environment, generally at depth in Earths crust. Origin of preexisting rock is mixed (for example, igneous and sedimentary) or is not known. Includes amphibolite, granulite, schist, and gneiss.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Marine sediment</edomv>
            <edomvd>Mud and sand, deposited in various marine environments. May originate from erosion of rocks and sediment or may be derived from marine organisms (of carbonate or siliceous composition).</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Quartzite</edomv>
            <edomvd>Rock derived from preexisting quartz-rich sedimentary rocks (commonly sandstone) and altered by essentially solid-state mineralogical, chemical, or structural changes, in response to marked changes in temperature, pressure, shear stress, and (or) chemical environment, generally at depth in Earths crust.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Ice-contact and ice-marginal sediment</edomv>
            <edomvd>Mostly sand-, silt-, and gravel-sized particles or clasts derived from rock or preexisting sediment that has been eroded and transported by glaciers. As glacier melted, material was deposited by running water essentially in contact with glacial ice or was transported and deposited by glacially fed streams. Includes sediment deposited into water bodies adjacent to glacier.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Glacial till, mostly silty</edomv>
            <edomvd>Mostly unsorted and unstratified material, generally unconsolidated, deposited directly by and underneath or adjacent to glacier without subsequent reworking by meltwater. Consists of heterogeneous mixture of clay, silt, sand, gravel, and boulders, ranging widely in size and shape. Relatively loamy (silty) in texture.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Loess</edomv>
            <edomvd>Silty sediment, deposited by wind, commonly near glacial margin.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Residual material</edomv>
            <edomvd>Unconsolidated material, developed in place by weathering of underlying rock or sediment. Usually forms relatively thin surface layer that conceals unweathered or partly altered source material. Material from which soils are formed.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Felsic-composition air-fall tephra</edomv>
            <edomvd>Fragments of volcanic rock and lava, of various sizes, carried into air by explosions and by hot gases in eruption columns or lava fountains; known as tephra. As tephra falls to ground, with increasing distance from volcano, average size of individual rock particles and thickness of resulting deposit decrease. Because of their high silica content and resulting high viscosity, felsic-composition magmas tend to erupt explosively, readily forming pumice and volcanic ash. Composed of light-colored rocks (for example, rhyolite, dacite, trachyte, latite).</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Dune sand</edomv>
            <edomvd>Mostly sand-sized sediment, deposited by wind. Typically characterized by various dune landforms.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Carbonate rock</edomv>
            <edomvd>Sedimentary rock, consisting chiefly of carbonate minerals such as limestone or dolomite.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Contact-metamorphic rock</edomv>
            <edomvd>Altered rock that originated by local processes of thermal metamorphism, genetically related to intrusion and extrusion of magmas and taking place at or near contact with body of igneous rock. Metamorphic changes are effected by heat and fluids emanating from magma and by some deformation because of emplacement of igneous mass.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Coarse-grained, mafic-composition intrusive igneous rock</edomv>
            <edomvd>Rock that solidified from molten or partly molten material (magma) at some depth beneath Earths surface, thereby cooling slowly enough for mineral crystals to grow large enough to be visible to naked eye. Composed mostly of feldspar and dark-colored minerals. Includes gabbroic rock.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Lava flows</edomv>
            <edomvd>Lateral, surficial outpourings of molten lava from vent or fissure; also, solidified bodies of rock that form when they cool. Composed generally of fine-grained, dark-colored rocks (for example, basalt), which tend to form extensive sheets that have generally low relief, except in vent areas where cinder cones or shield volcanoes may form. Includes basaltic shield volcanoes, which may become very large (for example, Hawaii).</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Air-fall tephra</edomv>
            <edomvd>Fragments of volcanic rock and lava, of various sizes, carried into air by explosions and by hot gases in eruption columns or lava fountains; known as tephra. As tephra falls to ground, with increasing distance from volcano, average size of individual rock particles and thickness of resulting deposit decrease. Fine tephra deposited at some distance from volcano is known as volcanic ash.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>"Made" or human-engineered land</edomv>
            <edomvd>Modern, unconsolidated material known to have human-related origin.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Glacial till, mostly sandy</edomv>
            <edomvd>Mostly unsorted and unstratified material, generally unconsolidated, deposited directly by and underneath or adjacent to glacier without subsequent reworking by meltwater. Consists of heterogeneous mixture of clay, silt, sand, gravel, and boulders, ranging widely in size and shape. Relatively sandy in texture.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Glacial till, mostly clayey</edomv>
            <edomvd>Mostly unsorted and unstratified material, generally unconsolidated, deposited directly by and underneath or adjacent to glacier without subsequent reworking by meltwater. Consists of heterogeneous mixture of clay, silt, sand, gravel, and boulders, ranging widely in size and shape. Relatively clayey in texture.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Coastal zone sediment, mostly coarse-grained</edomv>
            <edomvd>Mostly sand, silt, and gravel, deposited on beaches, in dunes, and in shallow-marine and related alluvial environments.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Felsic-composition lava flows</edomv>
            <edomvd>Lateral, surficial outpourings of molten lava from vent or fissure; also, solidified bodies of rock that form when they cool. Because of their high silica content and resulting high viscosity, parental magmas tend to erupt explosively, and so these deposits are uncommon. Includes fine-grained, light-colored rock with rhyolitic, dacitic, trachytic, and latitic composition.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Slate and phyllite, of sedimentary-rock origin</edomv>
            <edomvd>Fine-grained rock derived from preexisting sedimentary rocks and altered by essentially solid-state mineralogical, chemical, or structural changes, in response to marked changes in temperature, pressure, deformation, and (or) chemical environment, generally at depth in Earths crust. Includes phyllite and slate (compact, fine-grained rock that possesses strong cleavage and, hence, can be split into slabs and thin plates). Mostly formed from fine-grained material such as mudstone.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Fine-grained, felsic-composition intrusive igneous rock</edomv>
            <edomvd>Rock that solidified from molten or partly molten material (magma) at shallow depth beneath Earths surface, thereby cooling quickly. Generally fine grained but may contain large mineral crystals (phenocrysts). Mostly found as tabular dikes or sills. Composed mostly of light-colored minerals. Includes rhyolitic, dacitic, trachytic, and latitic rock.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Intermediate-composition air-fall tephra</edomv>
            <edomvd>Fragments of volcanic rock and lava, of various sizes, carried into the air by explosions and by hot gases in eruption columns or lava fountains; known as tephra. As tephra falls to ground, with increasing distance from volcano, average size of individual rock particles and thickness of resulting deposit decrease. Parental magma commonly erupts from stratovolcanoes as thick lava flows but also can generate strong explosive eruptions to form pyroclastic flows. Includes rocks that are, in color and mineral composition, intermediate between felsic and mafic rocks (for example, andesite).</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Chert</edomv>
            <edomvd>Sedimentary rock, composed chiefly of microcrystalline or cryptocrystalline quartz.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Mostly sandstone</edomv>
            <edomvd>Mostly sandstone, interbedded with other sedimentary rocks that locally may include conglomerate and finer grained clastic rocks (mudstone), carbonates, and (or) coal.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Sandstone</edomv>
            <edomvd>Sedimentary rock, composed predominantly of particles or clasts derived by erosion and weathering of preexisting rock; consists mostly of sand-sized particles, with or without fine-grained matrix of silt or clay.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Coarse-grained intrusive igneous rock</edomv>
            <edomvd>Rock that solidified from molten or partly molten material (magma) at some depth beneath Earths surface, thereby cooling slowly enough for mineral crystals to grow large enough to be visible to naked eye.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Rock and sediment</edomv>
            <edomvd>Various rocks and sediment, not differentiated.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Coarse-grained, felsic-composition intrusive igneous rock</edomv>
            <edomvd>Rock that solidified from molten or partly molten material (magma) at some depth beneath Earths surface, thereby cooling slowly enough for mineral crystals to grow large enough to be visible to naked eye. Composed mostly of light-colored minerals (for example, feldspar, quartz). Includes granitic, syenitic, and monzonitic rock.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Meta-mafic rock</edomv>
            <edomvd>Rock derived from preexisting mafic rocks by essentially solid-state, mineralogical, chemical, or structural changes, in response to marked changes in temperature, pressure, deformation, and (or) chemical environment, generally at depth in Earths crust. Composed mostly of iron- and magnesium-bearing, dark-colored and (or) green minerals. Includes greenstone, amphibolite, and metagabbro.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Meta-carbonate rock</edomv>
            <edomvd>Rock derived from preexisting carbonate sedimentary rocks and altered by essentially solid-state mineralogical, chemical, or structural changes, in response to marked changes in temperature, pressure, deformation, and (or) chemical environment, generally at depth in Earths crust. Characterized by recrystallization of carbonate minerals in source rock. Includes marble (for which preexisting rock was dominantly limestone or other rock composed of calcite), dolomitic marble, meta-dolostone, and meta-dolomite (for which preexisting rock contained appreciable amount of magnesium).</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Meta-volcaniclastic rock</edomv>
            <edomvd>Rock derived from preexisting volcaniclastic rocks by essentially solid-state, mineralogical, chemical, or structural changes, in response to marked changes in temperature, pressure, deformation, and (or) chemical environment, generally at depth in Earths crust. Composed of deformed but recognizable particles or clasts of volcanic explosive material.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Silt and clay of unspecified origin</edomv>
            <edomvd>Sediment composed mostly of silt and (or) clay, formed by weathering and erosion of preexisting rocks or minerals; eroded particles or clasts are transported and deposited by gravity, air, water, or ice.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Ice-contact and ice-marginal sediment, mostly coarse-grained</edomv>
            <edomvd>Mostly sand- and gravel-sized particles or clasts, with lesser amounts of silt and clay, derived from rock or preexisting sediment that has been eroded and transported by glaciers. As glacier melted, material was deposited by running water essentially in contact with glacial ice or was transported and deposited by glacially fed streams. Includes sediment deposited into water bodies adjacent to glacier.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Coal and lignite</edomv>
            <edomvd>Organic-rich sedimentary rock, formed from compaction and alteration of plant remains. Coal is consolidated, harder, black rock. Lignite is semiconsolidated, brown to black, earthy material that may contain large particles of recognizable plant parts and tends to crack upon drying.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Igneous and metamorphic rock</edomv>
            <edomvd>Consists of coarse-grained intrusive igneous rock and generally medium- to high-grade metamorphic rock.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Dolomite</edomv>
            <edomvd>Carbonate sedimentary rock, consisting chiefly of dolomite. Although dolostone is the proper analog to limestone, it has not often been applied to dolomitic units.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Other materials</edomv>
            <edomvd>Other materials</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Mostly carbonate rock</edomv>
            <edomvd>Mostly carbonate rock, interbedded with other sedimentary rock types.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Lower-grade metamorphic rock, of unspecified origin</edomv>
            <edomvd>Rock derived from preexisting rocks and altered by essentially solid-state mineralogical, chemical, or structural changes, in response to relatively mild regional changes in temperature, pressure, deformation, and (or) chemical environment, generally at depth in Earths crust. Origin of preexisting rock is mixed (for example, igneous and sedimentary) or is not known. Includes slate and phyllite.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Sedimentary and extrusive igneous material</edomv>
            <edomvd>Either (1) sedimentary rock and (or) unconsolidated material (sediment) and extrusive igneous material (volcanic rock and [or] sediment) or (2) volcanic rock and (or) sediment and such material after erosion and redeposition.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Sedimentary rock</edomv>
            <edomvd>Consolidated material (rock) composed of particles transported and deposited by gravity, air, water, or ice, or accumulated by other natural agents operating at Earths surface, such as chemical precipitation or secretion by organisms. Does not here include sedimentary material directly deposited as result of volcanic activity.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Glacial till</edomv>
            <edomvd>Mostly unsorted and unstratified material, generally unconsolidated, deposited directly by and underneath or adjacent to glacier without subsequent reworking by meltwater. Consists of heterogeneous mixture of clay, silt, sand, gravel, and boulders, ranging widely in size and shape.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Metasedimentary rock</edomv>
            <edomvd>Rock derived from preexisting sedimentary rocks and altered by essentially solid-state mineralogical, chemical, or structural changes, in response to marked changes in temperature, pressure, deformation, and (or) chemical environment, generally at depth in Earths crust.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Debris flows, landslides, and other localized mass-movement sediment</edomv>
            <edomvd>Sediment formed by relatively localized, downslope transport of particles or clasts produced by weathering and breakdown of underlying rock, sediment, and (or) soil. Composed of poorly sorted and poorly stratified material that ranges in size from clay to boulders. Speed of downslope transport ranges from rapid to imperceptible.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Conglomerate</edomv>
            <edomvd>Sedimentary rock, composed predominantly of particles or clasts derived by erosion and weathering of preexisting rock; contains more than 30 percent gravel-sized clasts.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Sediment</edomv>
            <edomvd>Unconsolidated material (sediment) composed of particles deposited by gravity, air, water, or ice, or as accumulated by other natural agents operating at Earths surface such as chemical precipitation or secretion by organisms. Does not include sedimentary material directly deposited as a result of volcanic activity.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Ice-contact and ice-marginal sediment, mostly fine-grained</edomv>
            <edomvd>Mostly silt- and clay-sized particles or clasts, with lesser amounts of sand and gravel, derived from rock or preexisting sediment that has been eroded and transported by glaciers. As glacier melted, material was deposited by running water essentially in contact with glacial ice or was transported and deposited by glacially fed streams. Includes sediment deposited into water bodies adjacent to glacier.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Coastal zone sediment</edomv>
            <edomvd>Mud and sand, with lesser amounts of gravel, deposited on beaches, on barrier islands, or in nearshore-marine, deltaic, or various low-energy shoreline (mud flat, tidal flat, sabka, algal flat) environments.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Volcaniclastic (fragmental) material</edomv>
            <edomvd>Rock and unconsolidated material consisting of particles or clasts that were formed by volcanic explosion or aerial expulsion from volcanic vent.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Evaporitic rock</edomv>
            <edomvd>Sedimentary rock, composed primarily of minerals produced by evaporation of saline solution. Examples include gypsum, anhydrite, other diverse sulfates, halite (rock salt), primary dolomite, and rocks composed of various nitrates and borates.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Eolian sediment</edomv>
            <edomvd>Silt- and sand-sized sediment, deposited by wind.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Peat and muck</edomv>
            <edomvd>Unconsolidated material, principally composed of plant remains, with lesser amounts of fine-grained clastic sediment. Deposited in water-saturated environment such as swamp, marsh, or bog. With lithification, such material becomes coal.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Mafic-composition air-fall tephra</edomv>
            <edomvd>Fragments of volcanic rock and lava, of various sizes, carried into the air by explosions and by hot gases in eruption columns or lava fountains; known as tephra. As tephra falls to ground, with increasing distance from volcano, average size of individual rock particles and thickness of resulting deposit decrease. Because of their low silica content and resulting low viscosity, parental magmas tend to erupt gently as lava flows, and so these deposits are uncommon. Includes basalt; rocks are commonly dark-colored.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Clastic sediment</edomv>
            <edomvd>Sediment formed by weathering and erosion of preexisting rocks or minerals; eroded particles or clasts are transported and deposited by gravity, air, water, or ice.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Extrusive igneous material</edomv>
            <edomvd>Molten material that was erupted onto Earths surface, fusing into rock or remaining as unconsolidated particles. Includes pyroclastic flows, air-fall tephra, lava flows, and volcanic mass flows.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Metamorphic rock</edomv>
            <edomvd>Rock derived from preexisting rocks and altered by essentially solid-state mineralogical, chemical, or structural changes, in response to marked changes in temperature, pressure, deformation, and (or) chemical environment, generally at depth in Earths crust.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Intermediate-composition lava flows</edomv>
            <edomvd>Lateral, surficial outpourings of molten lava from vent or fissure; also, solidified bodies of rock that form when they cool. Parental magma commonly erupts from stratovolcanoes as thick lava flows. Includes rocks that are, in color and in mineral composition, intermediate between felsic and mafic rocks (for example, andesite).</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Limestone</edomv>
            <edomvd>Carbonate sedimentary rock, consisting chiefly of calcite.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Clastic sedimentary rock</edomv>
            <edomvd>Sedimentary rock, composed predominantly of particles or clasts derived by erosion, weathering, or mass-wasting of preexisting rock and deposited by gravity, air, water, or ice.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Regional metamorphic rock, of unspecified origin</edomv>
            <edomvd>Rock derived from preexisting rocks and altered by essentially solid-state mineralogical, chemical, or structural changes, in response to marked regional changes in temperature, pressure, deformation, and (or) chemical environment, generally at depth in Earths crust. Origin of preexisting rock is mixed (for example, igneous and sedimentary) or is not known.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Mafic-composition pyroclastic flows</edomv>
            <edomvd>Hot ash, pumice, and rock fragments erupted from volcano. Material moves downslope commonly in chaotic flows; once deposited, hot fragments may compact under their own weight and weld together. Because of their low silica content and resulting low viscosity, parental magmas tend to erupt gently as lava flows rather than more forcefully as pyroclastic flows. Includes basalt; rocks are commonly dark-colored.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Meta-ultramafic rock</edomv>
            <edomvd>Rock derived from preexisting ultramafic rocks by essentially solid-state, mineralogical, chemical, or structural changes, in response to marked changes in temperature, pressure, deformation, and (or) chemical environment, generally at depth in Earths crust. Composed mostly of magnesium-bearing minerals (for example, serpentine, talc, magnesite).</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Alluvial sediment, mostly coarse-grained</edomv>
            <edomvd>Unconsolidated material deposited by streams or other bodies of running water as sorted or semisorted sediment in streambed, or on its floodplain or delta, or as cone or fan at base of mountain slope. Sediment is mostly sand, gravel, and coarser material but may also contain some silt and clay.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Lacustrine sediment</edomv>
            <edomvd>Mostly well-sorted and well-bedded material that ranges in grain size from clay to gravel, deposited in perennial to intermittent lakes. Much of sediment is derived from material eroded and transported by streams. Includes deposits of lake-marginal beaches and deltas.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Sand and gravel of unspecified origin</edomv>
            <edomvd>Sediment composed mostly of sand and (or) gravel, formed by weathering and erosion of preexisting rocks or minerals; eroded particles or clasts are transported and deposited by gravity, air, water, or ice.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Water or ice</edomv>
            <edomvd>Water or ice</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Schist and gneiss, of sedimentary-rock origin</edomv>
            <edomvd>Foliated rock derived from preexisting sedimentary rocks by essentially solid-state mineralogical, chemical, or structural changes in response to marked changes in temperature, pressure, deformation, and (or) chemical environment, generally at depth in Earths crust. Includes schist (characterized by such strong foliation or alignment of minerals that it readily splits into flakes or slabs) and gneiss (characterized by alternating, irregular bands of different mineral composition). Mostly formed from fine-grained material such as mudstone.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Intermediate-composition pyroclastic flows</edomv>
            <edomvd>Hot ash, pumice, and rock fragments erupted from volcano. Material moves downslope commonly in chaotic flows; once deposited, hot fragments may compact under their own weight and weld together. Parental magma commonly erupts from stratovolcanoes as thick lava flows but also can generate strong explosive eruptions to form pyroclastic flows. Includes rocks that are, in color and mineral composition, intermediate between felsic and mafic rocks (for example, andesite).</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Iron-rich sedimentary rock</edomv>
            <edomvd>Sedimentary rock, in which at least half (by volume) of observed minerals are iron bearing (hematite, magnetite, limonite group minerals, siderite, iron sulfides).</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Fine-grained intrusive igneous rock</edomv>
            <edomvd>Rock that solidified from molten or partly molten material (magma) at shallow depth beneath Earths surface, thereby cooling quickly. Generally fine grained but may contain large mineral crystals (phenocrysts). Mostly found as tabular dikes or sills.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Sedimentary material</edomv>
            <edomvd>An aggregation of particles deposited by gravity, air, water, or ice, or as accumulated by other natural agents operating at Earths surface such as chemical precipitation or secretion by organisms. May include unconsolidated material (sediment) and (or) sedimentary rock. Does not include sedimentary material directly deposited as a result of volcanic activity.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Alluvial sediment</edomv>
            <edomvd>Unconsolidated material deposited by streams or other bodies of running water as sorted or semisorted sediment in streambed, or on its floodplain or delta, or as cone or fan at base of mountain slope. Grain size varies from clay to gravel.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Fine-grained, intermediate-composition intrusive igneous rock</edomv>
            <edomvd>Rock that solidified from molten or partly molten material (magma) at shallow depth beneath Earths surface, thereby cooling quickly. Generally fine grained but may contain large mineral crystals (phenocrysts). Mostly found as tabular dikes or sills. Intermediate in color and in mineral composition (between felsic and mafic igneous rock). Includes andesitic rock.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Coastal zone sediment, mostly fine-grained</edomv>
            <edomvd>Mostly clay and silt, deposited in lagoons, tidal flats, backbarriers, and coastal marshes.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Mudstone</edomv>
            <edomvd>Sedimentary rock, composed predominantly of particles or clasts derived by erosion and weathering of preexisting rock; consists mostly of mud (that is, silt- and clay-sized particles). Includes shale and siltstone.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Deformation-related metamorphic rock</edomv>
            <edomvd>Rock derived from preexisting rocks by essentially solid-state mineralogical, chemical, or structural changes in response to strong deformation, commonly in association with marked changes in temperature, pressure, and (or) chemical environment. Generally forms in narrow, planar zones of local deformation (for example, along faults); characterized by foliation or alignment of mineral grains. Includes mylonite and cataclasite.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Mostly mudstone</edomv>
            <edomvd>Mostly mudstone, interbedded with other sedimentary rocks that locally may include coarser grained clastic rocks (sandstone, conglomerate), carbonates, and (or) coal.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Pyroclastic flows</edomv>
            <edomvd>Hot ash, pumice, and rock fragments erupted from volcano or caldera. Material moves downslope commonly in chaotic flows; once deposited, hot fragments may compact under their own weight and weld together.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Carbonate sediment</edomv>
            <edomvd>Sediment formed by biotic or abiotic precipitation from aqueous solution of carbonates of calcium, magnesium, or iron (for example, limestone, dolomite).</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Sandstone and mudstone</edomv>
            <edomvd>Sandstone and mudstone (including shale and siltstone), in approximately equal (or unspecified) proportions.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Exotic-composition intrusive igneous rock</edomv>
            <edomvd>Rock that solidified from molten or partly molten material (magma) below Earths surface that has exotic mineralogical, textural, or field setting characteristics. Typically dark colored with abundant phenocrysts. Includes kimberlite, lamprophyre, lamproite, and foiditic rocks.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Felsic-composition pyroclastic flows</edomv>
            <edomvd>Hot ash, pumice, and rock fragments erupted from volcano or caldera. Material moves downslope commonly in chaotic flows; once deposited, hot fragments may compact under their own weight and weld together. Because of their high-silica content and resulting high viscosity, parental magmas tend to erupt explosively. Includes rhyolite, dacite, trachyte, latite; rocks are commonly light-colored.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Unmapped area</edomv>
            <edomvd>Unmapped area</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Mafic-composition lava flows</edomv>
            <edomvd>Lateral, surficial outpourings of molten lava from vent or fissure; also, solidified bodies of rock that form when they cool. Low-silica parental magmas have low viscosity and tend to form extensive sheets that have generally low relief. Includes basaltic shield volcanoes, which may become very large (for example, in Hawaii). Composed of fine-grained, dark rocks, including basaltic.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Alluvial sediment, mostly fine-grained</edomv>
            <edomvd>Unconsolidated material deposited by streams or other bodies of running water as sorted or semisorted sediment in streambed, or on its floodplain or delta, or as cone or fan at base of mountain slope. Sediment is mostly silt and clay but may also contain some sand and gravel.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Playa sediment</edomv>
            <edomvd>Fine-grained clastic sediment and evaporitic salts, deposited in ephemeral lakes in centers of undrained basins. Includes material deposited in playas, mud flats, salt flats, and adjacent saline marshes. Generally interbedded with eolian sand and with lacustrine sediment deposited during wetter climatic periods; commonly intertongues upslope with sediment deposited by alluvial fans.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Rock</edomv>
            <edomvd>Various rock types, not differentiated.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Colluvium and other widespread mass-movement sediment</edomv>
            <edomvd>Sediment formed by slow, relatively widespread, downslope transport of particles or clasts produced by weathering and breakdown of underlying rock, sediment, and (or) soil. Composed of poorly sorted and poorly stratified material that ranges in size from clay to boulders.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Metaigneous rock</edomv>
            <edomvd>Rock derived from preexisting igneous rocks and altered by essentially solid-state, mineralogical, chemical, or structural changes, in response to marked changes in temperature, pressure, shear stress, and (or) chemical environment, generally at depth in Earths crust.</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Ultramafic intrusive igneous rock</edomv>
            <edomvd>Rock that solidified from molten or partly molten material (magma) at some depth beneath Earths surface, thereby cooling slowly enough for mineral crystals to grow large enough to be visible to naked eye. Composed almost entirely of mafic minerals (for example, hypersthene, augite, olivine).</edomvd>
            <edomvds>GeMS</edomvds>
          </edom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>IndentedName</attrlabl>
        <attrdef>Name with addition of leading spaces to help show rank within a hierarchical list.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Definition</attrlabl>
        <attrdef>Plain-language definition.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
    </detailed>
    <detailed>
      <enttyp>
        <enttypl>MapUnitPolys</enttypl>
        <enttypd>Polygons that record distribution of map units (including water, snowfields, glaciers, and unmapped area) on the particular map horizon.  In the original file geodatabase, this dataset is found within the GeologicMap feature dataset.</enttypd>
        <enttypds>GeMS</enttypds>
      </enttyp>
      <attr>
        <attrlabl>OBJECTID</attrlabl>
        <attrdef>Internal feature number</attrdef>
        <attrdefs>ESRI</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Shape</attrlabl>
        <attrdef>Internal geometry object</attrdef>
        <attrdefs>ESRI</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Shape_Length</attrlabl>
        <attrdef>Internal feature length, double</attrdef>
        <attrdefs>ESRI</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Shape_Area</attrlabl>
        <attrdef>Internal feature area, double</attrdef>
        <attrdefs>ESRI</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>MapUnit</attrlabl>
        <attrdef>Short plain-text identifier of the map unit. Foreign key to DescriptionOfMapUnits table.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <edom>
            <edomv>Sfa</edomv>
            <edomvd>Amphibolite member</edomvd>
            <edomvds>Walsh, G.J., 2016, Bedrock geologic map of the Hartland and North Hartland quadrangles, Windsor County, Vermont, and Sullivan and Grafton Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3361, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>DSwvf</edomv>
            <edomvd>Felsic volcanic member of the Waits River Formation</edomvd>
            <edomvds>BF24KNHVTDAS09 | BF24KNHVTDAS10</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Opv</edomv>
            <edomvd>Metafelsite volcanics and granofels member of the Partridge Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Ops</edomv>
            <edomvd>Pelitic schist and granofels member of the Partridge Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Dgqs</edomv>
            <edomvd>Gray quartzite and metapelite member of the Gile Mountain Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Srps</edomv>
            <edomvd>Porphyroblastic sillimanite schist member of the Rangeley Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>DSwsv</edomv>
            <edomvd>Metavolcaniclastic members of the Waits River Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Kd</edomv>
            <edomvd>Mafic dikes of the White Mountain Igneous Suite</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Dbg</edomv>
            <edomvd>Bethlehem Granodiorite of the New Hampshire Plutonic Suite</edomvd>
            <edomvds>BF24KNHVTDAS03 | BF24KNHVTDAS07 | BF24KNHVTDAS08</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Sf</edomv>
            <edomvd>Fitch Formation</edomvd>
            <edomvds>BF24KNHVTDAS12 | BF24KNHVTDAS08</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Oog</edomv>
            <edomvd>Granite gneiss of the Alstead dome</edomvd>
            <edomvds>BF24KNHVTDAS04 | BF24KNHVTDAS15</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Dg</edomv>
            <edomvd>Granite dikes of the New Hampshire Plutonic Suite</edomvd>
            <edomvds>Ratcliffe, N.M., Stanley, R.S., Gale, M.H., Thompson, P.J., and Walsh, G.J., 2011, Bedrock geologic map of Vermont: U.S. Geological Survey Scientific Investigations Map 3184, 3 sheets, scale 1:100,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Srq</edomv>
            <edomvd>Quartzite, calc-silicate, and schist member of the Rangeley Formation</edomvd>
            <edomvds>BF24KNHVTDAS14 | BF24KNHVTDAS07</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Scd</edomv>
            <edomvd>Metadiabase dikes of the Comerford Intrusive Complex</edomvd>
            <edomvds>Rankin, D.W., Coish, R.A., Tucker, R.D., Peng, Z.X., Wilson, S.A., and Rouff, A.A., 2007, Silurian extension in the upper Connecticut Valley, United States, and the origin of middle Paleozoic basins in the Québec embayment: American Journal of Science, v. 307, no. 1, p. 216–264.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>DSwg</edomv>
            <edomvd>Large-garnet and hornblende garbenscheifer schist member of the Waits River Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Dl</edomv>
            <edomvd>Littleton Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Sca</edomv>
            <edomvd>Amphibolite member of the Clough Quartzite</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Mzsz</edomv>
            <edomvd>Breccia or silicified zone</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>DSwhg</edomv>
            <edomvd>Hornblende-plagioclase gneiss member of the Waits River Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Dbd</edomv>
            <edomvd>Bethlehem quartz diorite of the New Hampshire Plutonic Suite</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Oaf</edomv>
            <edomvd>Intermediate to felsic metatuff member of the Ammonoosuc Volcanics</edomvd>
            <edomvds>BF24KNHVTDAS03 | BF24KNHVTDAS15</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Scs</edomv>
            <edomvd>Muscovite schist member of the Clough Quartzite</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>DSws</edomv>
            <edomvd>Gray phyllite and schist member of the Waits River Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Op</edomv>
            <edomvd>Rusty schist and granofels member of the Partridge Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>DSwa</edomv>
            <edomvd>Amphibolite and greenstone member of the Waits River Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>DSwr</edomv>
            <edomvd>Rusty schist member of the Waits River Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Oot</edomv>
            <edomvd>Trondhjemite gneiss of the Alstead dome</edomvd>
            <edomvds>BF24KNHVTDAS03 | BF24KNHVTDAS15</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Dgq</edomv>
            <edomvd>Feldspathic quartzite, granofels, and metapelite member of the Gile Mountain Formation</edomvd>
            <edomvds>Walsh, G.J., Valley, P.M., Armstrong, T.R., Ratcliffe, N.M., Merschat, A.J., and Gentry, B.J., 2020, Bedrock geologic map of the Springfield 7.5- x 15-minute quadrangle, Windsor County, Vermont, and Sullivan County, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3462, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Sfc</edomv>
            <edomvd>Metaconglomerate member of the Fitch Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>MDp</edomv>
            <edomvd>Muscovite-biotite pegmatite of the New Hampshire Plutonic suite</edomvd>
            <edomvds>Bradley, D.C., Shea, E., Buchwaldt, R., Bowring, S., Benowitz, J., O’Sullivan, P., and McCauley, A., 2016, Geochronology and tectonic context of lithium-cesium-tantalum pegmatites in the Appalachians: Canadian Mineralogist, v. 54, no. 4, p. 945–969.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Sr</edomv>
            <edomvd>Schist and granofels member of the Rangeley Formation</edomvd>
            <edomvds>BF24KNHVTDAS14 | BF24KNHVTDAS07</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>PSph</edomv>
            <edomvd>Phyllonite, undivided</edomvd>
            <edomvds>BF24KNHVTDAS02 | BF24KNHVTDAS03 | BF24KNHVTDAS04</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>DSwl</edomv>
            <edomvd>Limestone and schist member of the Waits River Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Scq</edomv>
            <edomvd>Quartzite and metaconglomerate member of the Clough Quartzite</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Opa</edomv>
            <edomvd>Amphibolite member of the Partridge Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Src</edomv>
            <edomvd>Metaconglomerate, granofels, and schist member of the Rangeley Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>DSwqc</edomv>
            <edomvd>Quartz-pebble to polymict conglomerate member of the Waits River Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>DSwvq</edomv>
            <edomvd>Metavolcaniclastic members of the Waits River Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>DSwv</edomv>
            <edomvd>Laminated schist and granofels member of the Waits River Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Oaa</edomv>
            <edomvd>Amphibolite member of the Ammonoosuc Volcanics</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>IdentityConfidence</attrlabl>
        <attrdef>Confidence that feature is correctly identified.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <edom>
            <edomv>certain</edomv>
            <edomvd>Identity of a feature can be determined using relevant observations and scientific judgment; therefore, one can be reasonably confident in the credibility of this interpretation.</edomvd>
            <edomvds>Federal Geographic Data Committee [prepared for the Federal Geographic Data Committee by the U.S. Geological Survey], 2006, FGDC Digital Cartographic Standard for Geologic Map Symbolization: Reston, Va., Federal Geographic Data Committee Document Number FGDC-STD-013-2006, 290 p., 2 plates.</edomvds>
          </edom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Label</attrlabl>
        <attrdef>Plain-text equivalent of the desired annotation for a feature: for example "14 Ma", or "^c" which (when used with the FGDC GeoAge font) results in the geologic map-unit label TRc (with TR run together to make the Triassic symbol).</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Symbol</attrlabl>
        <attrdef>Reference to a point marker, line symbol, or area-fill symbol that is used on the map graphic to denote the feature: perhaps a star for a K-Ar age locality, or a heavy black line for a fault.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>DataSourceID</attrlabl>
        <attrdef>Source of data; foreign key to table DataSources.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <edom>
            <edomv>BF24KNHVTDAS01</edomv>
            <edomvd>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvd>
            <edomvds>This report</edomvds>
          </edom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Notes</attrlabl>
        <attrdef>Additional information specific to a particular feature or table entry.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain. Free text. Values of &lt;null&gt; or #null indicate no entry.</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>MapUnitPolys_ID</attrlabl>
        <attrdef>Primary key.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Arbitrary string. Values should be unique within this database.</udom>
        </attrdomv>
      </attr>
    </detailed>
    <detailed>
      <enttyp>
        <enttypl>OverlayPolys</enttypl>
        <enttypd>Polygons that delineate underlying material, overlying material, or some aspect of earth materials other than the geologic map unit, e.g., dike swarm, alteration zone. On a map graphic, such polygons are commonly shown by a patterned overprint. In the original file geodatabase, this dataset is found within the GeologicMap feature dataset.</enttypd>
        <enttypds>GeMS</enttypds>
      </enttyp>
      <attr>
        <attrlabl>OBJECTID</attrlabl>
        <attrdef>Internal feature number</attrdef>
        <attrdefs>ESRI</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Shape</attrlabl>
        <attrdef>Internal geometry object</attrdef>
        <attrdefs>ESRI</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Shape_Length</attrlabl>
        <attrdef>Internal feature length, double</attrdef>
        <attrdefs>ESRI</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Shape_Area</attrlabl>
        <attrdef>Internal feature area, double</attrdef>
        <attrdefs>ESRI</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Type</attrlabl>
        <attrdef>Classifier that specifies what kind of geologic feature is represented by a database element: that a certain line within feature class ContactsAndFaults is a contact, or thrust fault, or water boundary; or that a point in GeochronPoints represents a K-Ar date.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <edom>
            <edomv>water body</edomv>
            <edomvd>Bodies of water in this database and accompanying published geologic map were delineated previously published base map material. They reside in the OverlayPolys feature class and were used to delineate concealed contacts and faults. Users of this database should note that the boundaries of these water bodies are not defined by modern methods such as LiDAR.</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>outcrop</edomv>
            <edomvd>Areas of exposed bedrock or closely spaced contiguous bedrock exposures examined in this study. Outcrops are exaggerated to show location on the published geologic map.</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>IdentityConfidence</attrlabl>
        <attrdef>Confidence that feature is correctly identified.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <edom>
            <edomv>certain</edomv>
            <edomvd>Identity of a feature can be determined using relevant observations and scientific judgment; therefore, one can be reasonably confident in the credibility of this interpretation.</edomvd>
            <edomvds>Federal Geographic Data Committee [prepared for the Federal Geographic Data Committee by the U.S. Geological Survey], 2006, FGDC Digital Cartographic Standard for Geologic Map Symbolization: Reston, Va., Federal Geographic Data Committee Document Number FGDC-STD-013-2006, 290 p., 2 plates.</edomvds>
          </edom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Label</attrlabl>
        <attrdef>Plain-text equivalent of the desired annotation for a feature: for example "14 Ma", or "^c" which (when used with the FGDC GeoAge font) results in the geologic map-unit label TRc (with TR run together to make the Triassic symbol).</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Symbol</attrlabl>
        <attrdef>Reference to a point marker, line symbol, or area-fill symbol that is used on the map graphic to denote the feature: perhaps a star for a K-Ar age locality, or a heavy black line for a fault.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>DataSourceID</attrlabl>
        <attrdef>Source of data; foreign key to table DataSources.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <edom>
            <edomv>BF24KNHVTDAS01</edomv>
            <edomvd>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvd>
            <edomvds>This report</edomvds>
          </edom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Notes</attrlabl>
        <attrdef>Additional information specific to a particular feature or table entry.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain. Free text. Values of &lt;null&gt; or #null indicate no entry.</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>OverlayPolys_ID</attrlabl>
        <attrdef>Primary key.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Arbitrary string. Values should be unique within this database.</udom>
        </attrdomv>
      </attr>
    </detailed>
    <detailed>
      <enttyp>
        <enttypl>ContactsAndFaults</enttypl>
        <enttypd>Contacts between map units, faults that bound map units, and associated dangling faults. Includes concealed faults and contacts, waterlines, snowfield and glacier boundaries, and map boundary. In the original file geodatabase, this dataset is found within the GeologicMap feature dataset.</enttypd>
        <enttypds>GeMS</enttypds>
      </enttyp>
      <attr>
        <attrlabl>OBJECTID</attrlabl>
        <attrdef>Internal feature number</attrdef>
        <attrdefs>ESRI</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Shape</attrlabl>
        <attrdef>Internal geometry object</attrdef>
        <attrdefs>ESRI</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Shape_Length</attrlabl>
        <attrdef>Internal feature length, double</attrdef>
        <attrdefs>ESRI</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Type</attrlabl>
        <attrdef>Classifier that specifies what kind of geologic feature is represented by a database element: that a certain line within feature class ContactsAndFaults is a contact, or thrust fault, or water boundary; or that a point in GeochronPoints represents a K-Ar date.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <edom>
            <edomv>map boundary</edomv>
            <edomvd>The line that surrounds a map, separating the map from the margin. Map boundaries usually consist of parallels and meridians, but conventional or arbitrary grid lines may be used.</edomvd>
            <edomvds>AGI | BF24KNHVTDAS01</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>contact</edomv>
            <edomvd>Trace of a plane or irregular surface between two types or ages of rock. All contacts within this map are approximate and concealed where water bodies are present</edomvd>
            <edomvds>Neuendorf, K.K.E., Mehl, J.P., Jr., and Jackson, J.A., eds., 2011, Glossary of geology (5th ed., revised): Alexandria, Va., American Geosciences Institute, 783 p.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>fault, metamorphic</edomv>
            <edomvd>Post-peak metamorphic strike-slip fault or shear zone; steeply dipping, parallel to the S2 foliation; paired arrows indicate relative left-lateral or right-lateral motion where known; U, upthrown side; D, downthrown side. Includes faults in the Westminster West fault zone and the Skitchewaug Mountain and Woodbury Road faults; likely created or reactivated during the Alleghanian orogeny. Approximately located; dotted where concealed by water. Queried where location is uncertain</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>fault, brittle</edomv>
            <edomvd>Steeply dipping fault in which the hanging wall has moved downward relative to the footwall; paired arrows indicate relative left-lateral or right-lateral motion where known; U, upthrown side; D, downthrown side. Includes the Ammonoosuc, Grantham, and Border faults; likely Paleozoic or Precambrian in age with reactivation during the Meosozoic era. Approximately located; dotted where concealed by water. Queried where location is uncertain</edomvd>
            <edomvds>AGI | BF24KNHVTDAS01</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>fault, thrust</edomv>
            <edomvd>Syn- to post-peak metamorphic thrust fault; parallel to the S2 foliation; sawteeth on upper plate. Includes the Fall Mountain thrust, the Brennan Hill thrust fault, and the Northey Hill fault; likely occurring during the Acadian or Alleghanian orogenies. Approximately located; dotted where concealed by water. Queried where location is uncertain</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>IsConcealed</attrlabl>
        <attrdef>Flag for contacts and faults covered by overlying map unit.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>LocationConfidenceMeters</attrlabl>
        <attrdef>Estimated half-width in meters of positional uncertainty envelope; position is relative to other features in database.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Positive real number. Value of -9, -99, or -999 indicates value is unknown.</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>ExistenceConfidence</attrlabl>
        <attrdef>Confidence that feature exists.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <edom>
            <edomv>certain</edomv>
            <edomvd>Identity of a feature can be determined using relevant observations and scientific judgment; therefore, one can be reasonably confident in the credibility of this interpretation.</edomvd>
            <edomvds>Federal Geographic Data Committee [prepared for the Federal Geographic Data Committee by the U.S. Geological Survey], 2006, FGDC Digital Cartographic Standard for Geologic Map Symbolization: Reston, Va., Federal Geographic Data Committee Document Number FGDC-STD-013-2006, 290 p., 2 plates.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>questionable</edomv>
            <edomvd>Identity of a feature cannot be determined using relevant observations and scientific judgment; therefore, one cannot be reasonably confident in the credibility of this interpretation. For example, IdentityConfidence = questionable is appropriate when a geologist reasons "I can see some kind of planar feature that separates map units in this outcrop, but I cannot be certain if it is a contact or a fault."</edomvd>
            <edomvds>Federal Geographic Data Committee [prepared for the Federal Geographic Data Committee by the U.S. Geological Survey], 2006, FGDC Digital Cartographic Standard for Geologic Map Symbolization: Reston, Va., Federal Geographic Data Committee Document Number FGDC-STD-013-2006, 290 p., 2 plates.</edomvds>
          </edom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>IdentityConfidence</attrlabl>
        <attrdef>Confidence that feature is correctly identified.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <edom>
            <edomv>certain</edomv>
            <edomvd>Identity of a feature can be determined using relevant observations and scientific judgment; therefore, one can be reasonably confident in the credibility of this interpretation.</edomvd>
            <edomvds>Federal Geographic Data Committee [prepared for the Federal Geographic Data Committee by the U.S. Geological Survey], 2006, FGDC Digital Cartographic Standard for Geologic Map Symbolization: Reston, Va., Federal Geographic Data Committee Document Number FGDC-STD-013-2006, 290 p., 2 plates.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>questionable</edomv>
            <edomvd>Identity of a feature cannot be determined using relevant observations and scientific judgment; therefore, one cannot be reasonably confident in the credibility of this interpretation. For example, IdentityConfidence = questionable is appropriate when a geologist reasons "I can see some kind of planar feature that separates map units in this outcrop, but I cannot be certain if it is a contact or a fault."</edomvd>
            <edomvds>Federal Geographic Data Committee [prepared for the Federal Geographic Data Committee by the U.S. Geological Survey], 2006, FGDC Digital Cartographic Standard for Geologic Map Symbolization: Reston, Va., Federal Geographic Data Committee Document Number FGDC-STD-013-2006, 290 p., 2 plates.</edomvds>
          </edom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Symbol</attrlabl>
        <attrdef>Reference to a point marker, line symbol, or area-fill symbol that is used on the map graphic to denote the feature: perhaps a star for a K-Ar age locality, or a heavy black line for a fault.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Label</attrlabl>
        <attrdef>Plain-text equivalent of the desired annotation for a feature: for example "14 Ma", or "^c" which (when used with the FGDC GeoAge font) results in the geologic map-unit label TRc (with TR run together to make the Triassic symbol).</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>DataSourceID</attrlabl>
        <attrdef>Source of data; foreign key to table DataSources.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <edom>
            <edomv>BF24KNHVTDAS01</edomv>
            <edomvd>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvd>
            <edomvds>This report</edomvds>
          </edom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Notes</attrlabl>
        <attrdef>Additional information specific to a particular feature or table entry.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain. Free text. Values of &lt;null&gt; or #null indicate no entry.</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>ContactsAndFaults_ID</attrlabl>
        <attrdef>Primary key.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Arbitrary string. Values should be unique within this database.</udom>
        </attrdomv>
      </attr>
    </detailed>
    <detailed>
      <enttyp>
        <enttypl>GeologicLines</enttypl>
        <enttypd>Lines that represent dikes, coal seams, ash beds, fold hinge-surface traces, isograds, and other linear features. All have these properties: (A) They do not participate in map-unit topology. (B) They correspond to features that exist within the Earth and may be concealed beneath younger, covering, material. (C) They are located with an accuracy that likely can be estimated. In the original file geodatabase, this dataset is found within the GeologicMap feature dataset.</enttypd>
        <enttypds>GeMS</enttypds>
      </enttyp>
      <attr>
        <attrlabl>OBJECTID</attrlabl>
        <attrdef>Internal feature number</attrdef>
        <attrdefs>ESRI</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Shape</attrlabl>
        <attrdef>Internal geometry object</attrdef>
        <attrdefs>ESRI</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Shape_Length</attrlabl>
        <attrdef>Internal feature length, double</attrdef>
        <attrdefs>ESRI</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Type</attrlabl>
        <attrdef>Classifier that specifies what kind of geologic feature is represented by a database element: that a certain line within feature class ContactsAndFaults is a contact, or thrust fault, or water boundary; or that a point in GeochronPoints represents a K-Ar date.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <edom>
            <edomv>syncline, overturned, F1</edomv>
            <edomvd>A fold of which the core contains the stratigraphically younger rocks; it is generally concave upward that has tilted beyond the perpendicular that likely occured during the Acadian orogeny (nappe-stage). Location is known or inferred; dotted where concealed by water. Symbols show trace of axial surface and direction of dip of limbs</edomvd>
            <edomvds>AGI | BF24KNHVTDAS01</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>metamorphic isograd</edomv>
            <edomvd>A line on a map joining points at which metamorphism proceeded at similar values of pressure and temperature as indicated by rocks containing a diagnostic mineral or mineral assemblage. Such a line represents the intersection of a reaction surface with the Earth's surface corresponding to the boundary between two contiguous zones of metamorphic grade, as defined by the appearance of specific index minerals, e.g., garnet isograd, staurolite isograd. Metamorphic isograds conincident with faults in this map have been removed. Notes in the ContactsandFaults feature class have been added to indicate a change in metamorphic assemblage coincident with those faults</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>antiform, overturned, F3</edomv>
            <edomvd>A convex-upward, concave downward fold that has tilted beyond the perpendicular likely occured during the later portion of the Alleghanian orogeny or even later during the Mesozoic age. Location is known or inferred; dotted where concealed by water. Symbols show trace of axial surface and direction of dip of limbs</edomvd>
            <edomvds>AGI | BF24KNHVTDAS01</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>synform, F3</edomv>
            <edomvd>A convex-downward, concave upward fold that likely occured during the later portion of the Alleghanian orogeny or even later during the Mesozoic age. Location is known or inferred; dotted where concealed by water. Symbols show trace of axial surface and direction of dip of limbs</edomvd>
            <edomvds>AGI | BF24KNHVTDAS01</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>antiform, F2</edomv>
            <edomvd>A convex-upward, concave downward fold that likely occrured during the early portion or during the Acadian orogeny. Location is known or inferred; dotted where concealed by water. Symbols show trace of axial surface and direction of dip of limbs; includes the Alstead dome that is not labeled on the published geologic map</edomvd>
            <edomvds>AGI | BF24KNHVTDAS01</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>synform, F2</edomv>
            <edomvd>A convex-downward, concave upward fold that likely occrured during the early portion or during the Acadian orogeny. Location is known or inferred; dotted where concealed by water. Symbols show trace of axial surface and direction of dip of limbs</edomvd>
            <edomvds>AGI | BF24KNHVTDAS01</edomvds>
          </edom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>IsConcealed</attrlabl>
        <attrdef>Flag for contacts and faults covered by overlying map unit.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>LocationConfidenceMeters</attrlabl>
        <attrdef>Estimated half-width in meters of positional uncertainty envelope; position is relative to other features in database.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Positive real number. Value of -9, -99, or -999 indicates value is unknown.</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>ExistenceConfidence</attrlabl>
        <attrdef>Confidence that feature exists.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <edom>
            <edomv>certain</edomv>
            <edomvd>Identity of a feature can be determined using relevant observations and scientific judgment; therefore, one can be reasonably confident in the credibility of this interpretation.</edomvd>
            <edomvds>Federal Geographic Data Committee [prepared for the Federal Geographic Data Committee by the U.S. Geological Survey], 2006, FGDC Digital Cartographic Standard for Geologic Map Symbolization: Reston, Va., Federal Geographic Data Committee Document Number FGDC-STD-013-2006, 290 p., 2 plates.</edomvds>
          </edom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>IdentityConfidence</attrlabl>
        <attrdef>Confidence that feature is correctly identified.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <edom>
            <edomv>certain</edomv>
            <edomvd>Identity of a feature can be determined using relevant observations and scientific judgment; therefore, one can be reasonably confident in the credibility of this interpretation.</edomvd>
            <edomvds>Federal Geographic Data Committee [prepared for the Federal Geographic Data Committee by the U.S. Geological Survey], 2006, FGDC Digital Cartographic Standard for Geologic Map Symbolization: Reston, Va., Federal Geographic Data Committee Document Number FGDC-STD-013-2006, 290 p., 2 plates.</edomvds>
          </edom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Symbol</attrlabl>
        <attrdef>Reference to a point marker, line symbol, or area-fill symbol that is used on the map graphic to denote the feature: perhaps a star for a K-Ar age locality, or a heavy black line for a fault.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Label</attrlabl>
        <attrdef>Plain-text equivalent of the desired annotation for a feature: for example "14 Ma", or "^c" which (when used with the FGDC GeoAge font) results in the geologic map-unit label TRc (with TR run together to make the Triassic symbol).</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>DataSourceID</attrlabl>
        <attrdef>Source of data; foreign key to table DataSources.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <edom>
            <edomv>BF24KNHVTDAS01</edomv>
            <edomvd>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvd>
            <edomvds>This report</edomvds>
          </edom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Notes</attrlabl>
        <attrdef>Additional information specific to a particular feature or table entry.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain. Free text. Values of &lt;null&gt; or #null indicate no entry.</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>GeologicLines_ID</attrlabl>
        <attrdef>Primary key.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Arbitrary string. Values should be unique within this database.</udom>
        </attrdomv>
      </attr>
    </detailed>
    <detailed>
      <enttyp>
        <enttypl>CartographicLines</enttypl>
        <enttypd>Lines (e.g., cross-section lines) that have no real-world physical existence, such that LocationConfidenceMeters, ExistenceConfidence, and IdentityConfidence attributes are meaningless, and that are never shown as concealed beneath a covering unit. In the original file geodatabase, this dataset is found within the GeologicMap feature dataset.</enttypd>
        <enttypds>GeMS</enttypds>
      </enttyp>
      <attr>
        <attrlabl>OBJECTID</attrlabl>
        <attrdef>Internal feature number</attrdef>
        <attrdefs>ESRI</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Shape</attrlabl>
        <attrdef>Internal geometry object</attrdef>
        <attrdefs>ESRI</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Shape_Length</attrlabl>
        <attrdef>Internal feature length, double</attrdef>
        <attrdefs>ESRI</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Type</attrlabl>
        <attrdef>Classifier that specifies what kind of geologic feature is represented by a database element: that a certain line within feature class ContactsAndFaults is a contact, or thrust fault, or water boundary; or that a point in GeochronPoints represents a K-Ar date.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <edom>
            <edomv>cross section</edomv>
            <edomvd>Surface line used to diagram or drawing that shows features transected by a given plane</edomvd>
            <edomvds>Neuendorf, K.K.E., Mehl, J.P., Jr., and Jackson, J.A., eds., 2011, Glossary of geology (5th ed., revised): Alexandria, Va., American Geosciences Institute, 783 p.</edomvds>
          </edom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Symbol</attrlabl>
        <attrdef>Reference to a point marker, line symbol, or area-fill symbol that is used on the map graphic to denote the feature: perhaps a star for a K-Ar age locality, or a heavy black line for a fault.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Label</attrlabl>
        <attrdef>Plain-text equivalent of the desired annotation for a feature: for example "14 Ma", or "^c" which (when used with the FGDC GeoAge font) results in the geologic map-unit label TRc (with TR run together to make the Triassic symbol).</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>DataSourceID</attrlabl>
        <attrdef>Source of data; foreign key to table DataSources.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <edom>
            <edomv>BF24KNHVTDAS01</edomv>
            <edomvd>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvd>
            <edomvds>This report</edomvds>
          </edom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Notes</attrlabl>
        <attrdef>Additional information specific to a particular feature or table entry.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain. Free text. Values of &lt;null&gt; or #null indicate no entry.</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>CartographicLines_ID</attrlabl>
        <attrdef>Primary key.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Arbitrary string. Values should be unique within this database.</udom>
        </attrdomv>
      </attr>
    </detailed>
    <detailed>
      <enttyp>
        <enttypl>OrientationPoints</enttypl>
        <enttypd>Point structure data (e.g., bedding attitudes, foliation attitudes, slip vectors measured at a point, etc.), one point per measurement. Multiple measurements at a single station (e.g., bedding and cleavage) should have the same StationsID. In the original file geodatabase, this dataset is found within the GeologicMap feature dataset.</enttypd>
        <enttypds>GeMS</enttypds>
      </enttyp>
      <attr>
        <attrlabl>OBJECTID</attrlabl>
        <attrdef>Internal feature number</attrdef>
        <attrdefs>ESRI</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Shape</attrlabl>
        <attrdef>Internal geometry object</attrdef>
        <attrdefs>ESRI</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Type</attrlabl>
        <attrdef>Classifier that specifies what kind of geologic feature is represented by a database element: that a certain line within feature class ContactsAndFaults is a contact, or thrust fault, or water boundary; or that a point in GeochronPoints represents a K-Ar date.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <edom>
            <edomv>dike and (or) sill, Kd</edomv>
            <edomvd>Structural measurement of tabular igneous intrusions of Cretaceous age mafic dikes [Kd} that cuts across or are parallel to the bedding or foliation of country rock</edomvd>
            <edomvds>AGI | BF24KNHVTDAS01</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>lineation, stretched pebble</edomv>
            <edomvd>Structural measurement defined by the long axis of a deformed elongate pebble; measurement taken where deformed pebbles have similar oriented long axes</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>axial surface, F2</edomv>
            <edomvd>Structural measurement of a surface that connects the hinge line of tightly folded rootless (isoclinal) strata likely during the beginning or during the Acadian orogeny (dome-stage). F2 folds are parallel to S2 foliation</edomvd>
            <edomvds>AGI | BF24KNHVTDAS01</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>fold axis, F1</edomv>
            <edomvd>Structural measurement of a line connecting the points of flexure or maximum curvature of (beds, foliation) in tight (isoclinal) folds formed during the beginning or during the Acadian orogeny (dome-stage)</edomvd>
            <edomvds>AGI | BF24KNHVTDAS01</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>dike and (or) sill, Scd</edomv>
            <edomvd>Structural measurement of a tabular igneous intrusions of Silurian age metadiabase dikes of the Comerford Intrusive Complex [Scd] that cuts across or are parallel to the bedding or foliation of the country rock</edomvd>
            <edomvds>AGI | BF24KNHVTDAS01</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>axial surface, F1</edomv>
            <edomvd>Structural measurement of a surface that connects the hinge line of tightly folded rootless (isoclinal) strata likely during the end of the Acadian orogeny (nappe-stage). F1 folds are parallel to S1 foliation.</edomvd>
            <edomvds>AGI | BF24KNHVTDAS01</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>fold axis, F2</edomv>
            <edomvd>Structural measurement of a line connecting the points of flexure or maximum curvature of (beds, foliation) in tight (isoclinal) folds formed during the late Acadian orogeny (dome-stage)</edomvd>
            <edomvds>AGI | BF24KNHVTDAS01</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>kink band</edomv>
            <edomvd>Structural measurement of a non-penetrative widely spaced cleavage, locally parallel to broad low-amplitude, high-wavelength folds with variable orientation; locally quartz and carbonate mineralization fills veins parallel to kink surfaces; may be related to brittle faults and Mesozoic extension</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>foliation, spaced, S2</edomv>
            <edomvd>Structural measurement of a planar arrangement of textural or structural features in schist or other metamorphic or igneous rock, a preferred orientation of crystal planes in mineral grains, a preferred orientation of inequant grain shapes, or from compositional banding. Likely formed during the Acadian orogeny but may have formed during later mountain building events</edomvd>
            <edomvds>AGI | BF24KNHVTDAS01M</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>lineation, mineral, L2</edomv>
            <edomvd>Structural measurement of a linear fabric element defined by the preferred orientation of inequant mineral grains or elongated grain aggregates frequently associated with foliations formed during the Acadian orogen consisting of quartz, plagioclase, biotite, muscovite, chlorite, or amphibole</edomvd>
            <edomvds>AGI | BF24KNHVTDAS01</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>lineation, intersection, L2</edomv>
            <edomvd>Structural measurement of a lineation formed by the intersection of two planar surfaces, at least one of which is penetrative associated with foliation that occured during differing times of the Acadian orogeny or possibly Alleghanian orogeny</edomvd>
            <edomvds>AGI | BF24KNHVTDAS01</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>dike and (or) sill, Oot</edomv>
            <edomvd>Structural measurement of a tabular igneous intrusions of Ordovician age Trondhjemite gneiss of the Alstead dome [Oot] that cuts across or are parallel to the bedding or foliation of the country rock</edomvd>
            <edomvds>AGI | BF24KNHVTDAS01</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>layer-parallel foliation, S1</edomv>
            <edomvd>Structural measurement of a folded pattern of parallel layers of minerals in metamorphic rocks that occurs when minerals align and recrystallize</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>joint</edomv>
            <edomvd>Structural measurement of a planar fracture, crack, or parting in a rock, without shear displacement</edomvd>
            <edomvds>Neuendorf, K.K.E., Mehl, J.P., Jr., and Jackson, J.A., eds., 2011, Glossary of geology (5th ed., revised): Alexandria, Va., American Geosciences Institute, 783 p.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>cleavage, S2</edomv>
            <edomvd>Structural measurement of a locally planar fabric in an unmetamorphosed or weakly metamorphosed, fine-grained rock defined by either the tendency of a rock to split in a particular direction, a preferred orientation of crystal planes in mineral grains, or a preferred orientation of inequant grain shapes. Penetrative to the west, zonal in the east; likely formed during the Acadian orogeny</edomvd>
            <edomvds>AGI | BF24KNHVTDAS01</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>dike and (or) sill, Dg</edomv>
            <edomvd>Structural measurement of a tabular igneous intrusions of Devonian age granite dikes [Dg] that cut across or are parallel to the bedding or foliation of  country rock</edomvd>
            <edomvds>AGI | BF24KNHVTDAS01</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>fold axis and (or) crenulation lineation, F3</edomv>
            <edomvd>Structural measurement of a line connecting the points of flexure or maximum curvature of (beds, foliation) in open folds during the late Alleghanian orogeny late dome-stage or younger</edomvd>
            <edomvds>AGI | BF24KNHVTDAS01</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>cleavage, S3</edomv>
            <edomvd>Structural measurement of a foliation that results from a preferred orientation of rock layers or mineral grains due to microscale folding. Associated with open folds and a crenulation lineation that is most apparent in fine-grained metapelites of the Alleghanian orogeny</edomvd>
            <edomvds>AGI | BF24KNHVTDAS01</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>lineation, folded</edomv>
            <edomvd>Structural measurement of a linear fabric element defined by the preferred orientation of inequant mineral grains (e.g. prismatic grains of hornblende) or elongated grain aggregates. This lineation was clearly folded</edomvd>
            <edomvds>AGI | BF24KNHVTDAS01</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>dike and (or) sill, MDp</edomv>
            <edomvd>Structural measurement of a tabular igneous intrusions of Mississippian to Devonian age muscovite-biotite pegmatite (MDp) that cuts across or are parallel to the bedding or foliation of country rock</edomvd>
            <edomvds>AGI | BF24KNHVTDAS01</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>fold axis, folded, F1</edomv>
            <edomvd>Structural measurement of a line connecting the points of flexure or maximum curvature of (beds, foliation) in tight (isoclinal) folds formed during the beginning or during the Acadian orogeny (dome-stage); this single measurement was refolded presumably during the Alleghanian orogeny or later</edomvd>
            <edomvds>AGI | BF24KNHVTDAS01</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>axial surface, F3</edomv>
            <edomvd>Structural measurement of a surface that connects the hinge line of openly folded strata during the Alleghanian orogeny</edomvd>
            <edomvds>AGI | BF24KNHVTDAS01</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>foliation, mylonitic, S2</edomv>
            <edomvd>Structural measurement of a planar arrangement of textural or structural features in mylonitic or phyllonitic rock near shear zones likely occuring during the Acadian orogeny</edomvd>
            <edomvds>AGI | BF24KNHVTDAS01</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>slickenside</edomv>
            <edomvd>Structural measurement of a lineation defined by grooves, ridges, and/or striations along a fault surface</edomvd>
            <edomvds>Neuendorf, K.K.E., Mehl, J.P., Jr., and Jackson, J.A., eds., 2011, Glossary of geology (5th ed., revised): Alexandria, Va., American Geosciences Institute, 783 p.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>vein</edomv>
            <edomvd>Structural measurement of quartz veins. Width of the features in this type are displayed in the Width field of the OrientationPoints feature class.</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>glacial grooves</edomv>
            <edomvd>Structural measurement of a deep, wide, usually straight furrow cut in bedrock by the abrasive action of a rock fragment embedded in the bottom of a moving glacier</edomvd>
            <edomvds>Neuendorf, K.K.E., Mehl, J.P., Jr., and Jackson, J.A., eds., 2011, Glossary of geology (5th ed., revised): Alexandria, Va., American Geosciences Institute, 783 p.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>foliation, Sn</edomv>
            <edomvd>Structural measurement of a planar arrangement of textural or structural features in any type of rock, esp. the locally planar fabric in a rock defined by a fissility, a preferred orientation of crystal planes in mineral grains, a preferred orientation of inequant grain shapes, or from compositional banding. Likely formed during the Acadian orogeny but may have formed during later mountain building events</edomvd>
            <edomvds>AGI | BF24KNHVTDAS01</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>shear band</edomv>
            <edomvd>Structural measurement of a foliation caused by the shearing of rock due to intense strain in parallel or sub-parallel directions</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>fault</edomv>
            <edomvd>Structural measurement of a local discrete surface or zone of discrete surfaces separating two rock masses across which one mass has slid past the other. Direction of local faulting structural measurements, where known, were characterized in the FaultType field in the OrientationPoints features class in this database</edomvd>
            <edomvds>AGI | BF24KNHVTDAS01</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>foliation, deformed, S1</edomv>
            <edomvd>Structural measurement of a deformed planar arrangement of textural or structural features in any type of rock, esp. the locally planar fabric in a rock defined by a fissility, a preferred orientation of crystal planes in mineral grains, a preferred orientation of inequant grain shapes, or from compositional banding. Likely formed during the Acadian orogeny</edomvd>
            <edomvds>AGI | BF24KNHVTDAS01</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>bedding</edomv>
            <edomvd>Structural measurement of the arrangement of inclined or overturned sedimentary or? igneous rocks in beds or layers of varying thickness and character. This attribute contains structural measurements with crossbedding and graded bedding used a younging indicators</edomvd>
            <edomvds>AGI | BF24KNHVTDAS01</edomvds>
          </edom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Azimuth</attrlabl>
        <attrdef>Strike or trend, measured in degrees clockwise from geographic North. Use right-hand rule (dip is to right of azimuth direction). Horizontal planar features may have any azimuth.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <rdom>
            <rdommin>0</rdommin>
            <rdommax>360</rdommax>
            <attrunit>degrees (angular measure)</attrunit>
          </rdom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Inclination</attrlabl>
        <attrdef>Dip or plunge, measured in degrees down from horizontal. Negative values allowed when specifying vectors (not axes) that point above the horizon, e.g., paleocurrents. Types defined as horizontal (e.g., horizontal bedding) shall have Inclination=0.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <rdom>
            <rdommin>-90</rdommin>
            <rdommax>90</rdommax>
            <attrunit>degrees (angular measure)</attrunit>
          </rdom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Symbol</attrlabl>
        <attrdef>Reference to a point marker, line symbol, or area-fill symbol that is used on the map graphic to denote the feature: perhaps a star for a K-Ar age locality, or a heavy black line for a fault.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Label</attrlabl>
        <attrdef>Plain-text equivalent of the desired annotation for a feature: for example "14 Ma", or "^c" which (when used with the FGDC GeoAge font) results in the geologic map-unit label TRc (with TR run together to make the Triassic symbol).</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>LocationConfidenceMeters</attrlabl>
        <attrdef>Estimated half-width in meters of positional uncertainty envelope; position is relative to other features in database.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Positive real number. Value of -9, -99, or -999 indicates value is unknown.</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>IdentityConfidence</attrlabl>
        <attrdef>Confidence that feature is correctly identified.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <edom>
            <edomv>certain</edomv>
            <edomvd>Identity of a feature can be determined using relevant observations and scientific judgment; therefore, one can be reasonably confident in the credibility of this interpretation.</edomvd>
            <edomvds>Federal Geographic Data Committee [prepared for the Federal Geographic Data Committee by the U.S. Geological Survey], 2006, FGDC Digital Cartographic Standard for Geologic Map Symbolization: Reston, Va., Federal Geographic Data Committee Document Number FGDC-STD-013-2006, 290 p., 2 plates.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>questionable</edomv>
            <edomvd>Identity of a feature cannot be determined using relevant observations and scientific judgment; therefore, one cannot be reasonably confident in the credibility of this interpretation. For example, IdentityConfidence = questionable is appropriate when a geologist reasons "I can see some kind of planar feature that separates map units in this outcrop, but I cannot be certain if it is a contact or a fault."</edomvd>
            <edomvds>Federal Geographic Data Committee [prepared for the Federal Geographic Data Committee by the U.S. Geological Survey], 2006, FGDC Digital Cartographic Standard for Geologic Map Symbolization: Reston, Va., Federal Geographic Data Committee Document Number FGDC-STD-013-2006, 290 p., 2 plates.</edomvds>
          </edom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>OrientationConfidenceDegrees</attrlabl>
        <attrdef>Estimated angular precision of combined azimuth AND inclination measurements, in degrees.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Positive real number. Value of -9, -99, or -999 indicates value is unknown.</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>PlotAtScale</attrlabl>
        <attrdef>At what scale (or larger) should this observation or analysis be plotted? At smaller scales, it should not be plotted. Useful to prevent crowding of display at small scales and to display progressively more data at larger and larger scales. Value is scale denominator.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Positive real number.</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>StationsID</attrlabl>
        <attrdef>Station number assigned by person who 
originally located this station. Commonly, 
key to field sheet, field, or digital notebook.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>MapUnit</attrlabl>
        <attrdef>Short plain-text identifier of the map unit. Foreign key to DescriptionOfMapUnits table.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <edom>
            <edomv>DSwvf</edomv>
            <edomvd>Felsic volcanic member of the Waits River Formation</edomvd>
            <edomvds>BF24KNHVTDAS09 | BF24KNHVTDAS10</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Opv</edomv>
            <edomvd>Metafelsite volcanics and granofels member of the Partridge Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Ops</edomv>
            <edomvd>Pelitic schist and granofels member of the Partridge Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Dgqs</edomv>
            <edomvd>Gray quartzite and metapelite member of the Gile Mountain Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Srps</edomv>
            <edomvd>Porphyroblastic sillimanite schist member of the Rangeley Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>DSwsv</edomv>
            <edomvd>Metavolcaniclastic members of the Waits River Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Kd</edomv>
            <edomvd>Mafic dikes of the White Mountain Igneous Suite</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Dbg</edomv>
            <edomvd>Bethlehem Granodiorite of the New Hampshire Plutonic Suite</edomvd>
            <edomvds>BF24KNHVTDAS03 | BF24KNHVTDAS07 | BF24KNHVTDAS08</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Sf</edomv>
            <edomvd>Fitch Formation</edomvd>
            <edomvds>BF24KNHVTDAS12 | BF24KNHVTDAS08</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Oog</edomv>
            <edomvd>Granite gneiss of the Alstead dome</edomvd>
            <edomvds>BF24KNHVTDAS04 | BF24KNHVTDAS15</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>DSwv</edomv>
            <edomvd>Laminated schist and granofels member of the Waits River Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Dg</edomv>
            <edomvd>Granite dikes of the New Hampshire Plutonic Suite</edomvd>
            <edomvds>Ratcliffe, N.M., Stanley, R.S., Gale, M.H., Thompson, P.J., and Walsh, G.J., 2011, Bedrock geologic map of Vermont: U.S. Geological Survey Scientific Investigations Map 3184, 3 sheets, scale 1:100,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Srq</edomv>
            <edomvd>Quartzite, calc-silicate, and schist member of the Rangeley Formation</edomvd>
            <edomvds>BF24KNHVTDAS14 | BF24KNHVTDAS07</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Scd</edomv>
            <edomvd>Metadiabase dikes of the Comerford Intrusive Complex</edomvd>
            <edomvds>Rankin, D.W., Coish, R.A., Tucker, R.D., Peng, Z.X., Wilson, S.A., and Rouff, A.A., 2007, Silurian extension in the upper Connecticut Valley, United States, and the origin of middle Paleozoic basins in the Québec embayment: American Journal of Science, v. 307, no. 1, p. 216–264.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>DSwg</edomv>
            <edomvd>Large-garnet and hornblende garbenscheifer schist member of the Waits River Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Sca</edomv>
            <edomvd>Amphibolite member of the Clough Quartzite</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Mzsz</edomv>
            <edomvd>Breccia or silicified zone</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>DSwhg</edomv>
            <edomvd>Hornblende-plagioclase gneiss member of the Waits River Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Dbd</edomv>
            <edomvd>Bethlehem quartz diorite of the New Hampshire Plutonic Suite</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Oaf</edomv>
            <edomvd>Intermediate to felsic metatuff member of the Ammonoosuc Volcanics</edomvd>
            <edomvds>BF24KNHVTDAS03 | BF24KNHVTDAS15</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Scs</edomv>
            <edomvd>Muscovite schist member of the Clough Quartzite</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>DSws</edomv>
            <edomvd>Gray phyllite and schist member of the Waits River Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Op</edomv>
            <edomvd>Rusty schist and granofels member of the Partridge Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>DSwa</edomv>
            <edomvd>Amphibolite and greenstone member of the Waits River Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>DSwr</edomv>
            <edomvd>Rusty schist member of the Waits River Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Oot</edomv>
            <edomvd>Trondhjemite gneiss of the Alstead dome</edomvd>
            <edomvds>BF24KNHVTDAS03 | BF24KNHVTDAS15</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Dgq</edomv>
            <edomvd>Feldspathic quartzite, granofels, and metapelite member of the Gile Mountain Formation</edomvd>
            <edomvds>Walsh, G.J., Valley, P.M., Armstrong, T.R., Ratcliffe, N.M., Merschat, A.J., and Gentry, B.J., 2020, Bedrock geologic map of the Springfield 7.5- x 15-minute quadrangle, Windsor County, Vermont, and Sullivan County, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3462, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Sfc</edomv>
            <edomvd>Metaconglomerate member of the Fitch Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>MDp</edomv>
            <edomvd>Muscovite-biotite pegmatite of the New Hampshire Plutonic suite</edomvd>
            <edomvds>Bradley, D.C., Shea, E., Buchwaldt, R., Bowring, S., Benowitz, J., O’Sullivan, P., and McCauley, A., 2016, Geochronology and tectonic context of lithium-cesium-tantalum pegmatites in the Appalachians: Canadian Mineralogist, v. 54, no. 4, p. 945–969.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Sr</edomv>
            <edomvd>Schist and granofels member of the Rangeley Formation</edomvd>
            <edomvds>BF24KNHVTDAS14 | BF24KNHVTDAS07</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>PSph</edomv>
            <edomvd>Phyllonite, undivided</edomvd>
            <edomvds>BF24KNHVTDAS02 | BF24KNHVTDAS03 | BF24KNHVTDAS04</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>DSwl</edomv>
            <edomvd>Limestone and schist member of the Waits River Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Scq</edomv>
            <edomvd>Quartzite and metaconglomerate member of the Clough Quartzite</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Opa</edomv>
            <edomvd>Amphibolite member of the Partridge Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Src</edomv>
            <edomvd>Metaconglomerate, granofels, and schist member of the Rangeley Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>DSwqc</edomv>
            <edomvd>Quartz-pebble to polymict conglomerate member of the Waits River Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>DSwvq</edomv>
            <edomvd>Metavolcaniclastic members of the Waits River Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Dl</edomv>
            <edomvd>Littleton Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Oaa</edomv>
            <edomvd>Amphibolite member of the Ammonoosuc Volcanics</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>LocationSourceID</attrlabl>
        <attrdef>Source of location; foreign key to table DataSources.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <edom>
            <edomv>BF24KNHVTDAS01</edomv>
            <edomvd>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvd>
            <edomvds>This report</edomvds>
          </edom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>OrientationSourceID</attrlabl>
        <attrdef>Source of orientation data; foreign key to table DataSources.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <edom>
            <edomv>BF24KNHVTDAS01</edomv>
            <edomvd>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvd>
            <edomvds>This report</edomvds>
          </edom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Notes</attrlabl>
        <attrdef>Additional information specific to a particular feature or table entry.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain. Free text. Values of &lt;null&gt; or #null indicate no entry.</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>OrientationPoints_ID</attrlabl>
        <attrdef>Primary key.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Arbitrary string. Values should be unique within this database.</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Parting</attrlabl>
        <attrdef>"Y" Indicates the planar feature exhibits parting or fracturing parallel to the surface measured. Null values indicate the structural measurement does not have parting or the field does not apply to that measurement.</attrdef>
        <attrdefs>BF24KNHVTDAS01</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Throughgoing</attrlabl>
        <attrdef>"Y" indicates the measured brittle feature is throughgoing and passes through the entire outcrop. Null values indicate the structural measurement is not throughgoing or the field does not apply to that measurement.</attrdef>
        <attrdefs>BF24KNHVTDAS01</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Fracture</attrlabl>
        <attrdef>"Y" indicates feature is a fracture. Null values indicate the structural measurement does not have fracture or the field does not apply to that measurement.</attrdef>
        <attrdefs>BF24KNHVTDAS01</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Termination</attrlabl>
        <attrdef>Termination of joints where known. Null values indicate the structural measurement has an unknown termination value or the field does not apply to that measurement.</attrdef>
        <attrdefs>BF24KNHVTDAS01</attrdefs>
        <attrdomv>
          <edom>
            <edomv>crossing</edomv>
            <edomvd>Joint has created some visible displacement in outcrop.</edomvd>
            <edomvds>BF24KNHVTDAS01</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>blind</edomv>
            <edomvd>Joint has created no visible displacement in outcrop or displacement is unknown or undecipherable in outcrop.</edomvd>
            <edomvds>BF24KNHVTDAS01</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>abutting</edomv>
            <edomvd>Joint has created no visible displacement in outcrop.</edomvd>
            <edomvds>Producer defined</edomvds>
          </edom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Width</attrlabl>
        <attrdef>Numeric width or thickness of dike and (or) vein; units in meters range from 50 to 0.001. Null values indicate lack of measurement or the field does not apply to that measurement.</attrdef>
        <attrdefs>BF24KNHVTDAS01</attrdefs>
        <attrdomv>
          <rdom>
            <rdommin>.001</rdommin>
            <rdommax>50</rdommax>
            <attrunit>meters</attrunit>
          </rdom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>FaultType</attrlabl>
        <attrdef>Movement sense of brittle fault as measured in local outcrop. Null values indicate fault movement is unknown or the field does not apply to that measurement.</attrdef>
        <attrdefs>BF24KNHVTDAS01</attrdefs>
        <attrdomv>
          <edom>
            <edomv>reverse</edomv>
            <edomvd>Indicates the movement of the local fault measurements is reverse.</edomvd>
            <edomvds>BF24KNHVTDAS01</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>thrust</edomv>
            <edomvd>Indicates the movement of the local fault measurements is thrust.</edomvd>
            <edomvds>BF24KNHVTDAS01</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>normal</edomv>
            <edomvd>Indicates the movement of the local fault measurements is normal.</edomvd>
            <edomvds>BF24KNHVTDAS01</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>right lateral</edomv>
            <edomvd>Indicates the movement of the local fault measurements is dextral.</edomvd>
            <edomvds>BF24KNHVTDAS01</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>left lateral</edomv>
            <edomvd>Indicates the movement of the local fault measurements is sinistral.</edomvd>
            <edomvds>BF24KNHVTDAS01</edomvds>
          </edom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Mineral</attrlabl>
        <attrdef>Primary mineral in veins or metamorphic index minerals; valid values include: tourmaline, sulfide, staurolite, sillimanite, quartz, pyrite, plagioclase, magnetite, hornblende, garnet, epidote, chlorite, chaccopyrite, biotite, alkali feldspar, and actinolite. Null values indicate lack of information or the field does not apply to that measurement.</attrdef>
        <attrdefs>BF24KNHVTDAS01</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>SymbolX</attrlabl>
        <attrdef>Modified FGDC reference values for structural measurements within the OrientationPoints feature class. Values of .01 and .02 following tradtional FGDC values shift the cartographic symbol to the left or right easing cartographic production. Additional modifications including changes to individual reference value cartographic specifications to create new symbols for use on the published geologic map. The most common change is to reference value 08.02.11 (inclined cumulate foliation) by adding additional fill colors by creating a "box" with the symbol. This field allows the user of this database to "match symbols to a syle" from the custom FGDC styleX file provided with the database; allowing total reproduction of the structural measurement symbols on the published geologic map.</attrdef>
        <attrdefs>BF24KNHVTDAS01</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
    </detailed>
    <detailed>
      <enttyp>
        <enttypl>GeochronPoints</enttypl>
        <enttypd>Point locations of samples and accompanying geochronological measurements. Type field identifies geochronological method.</enttypd>
        <enttypds>GeMS</enttypds>
      </enttyp>
      <attr>
        <attrlabl>OBJECTID</attrlabl>
        <attrdef>Internal feature number</attrdef>
        <attrdefs>ESRI</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Shape</attrlabl>
        <attrdef>Internal geometry object</attrdef>
        <attrdefs>ESRI</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Type</attrlabl>
        <attrdef>Classifier that specifies what kind of geologic feature is represented by a database element: that a certain line within feature class ContactsAndFaults is a contact, or thrust fault, or water boundary; or that a point in GeochronPoints represents a K-Ar date.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <edom>
            <edomv>Ar/Ar geochronology</edomv>
            <edomvd>Sample location of age dated rock from a variation of the potassium-argon age method in which the sample to be dated is first irradiated with neutrons, converting some potassium-39 to argon-39. Argon is then extracted from the sample (either in one step or incrementally), and its isotopic composition analyzed. The amount of argon-39 is a measure of potassium content, and the ratio of radiogenic argon-40 to argon-39 is a function of age</edomvd>
            <edomvds>Neuendorf, K.K.E., Mehl, J.P., Jr., and Jackson, J.A., eds., 2011, Glossary of geology (5th ed., revised): Alexandria, Va., American Geosciences Institute, 783 p.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>SHRIMP geochronology</edomv>
            <edomvd>Sample location of age dated rock using the sensitive high resolution ion microprobe (SHRIMP) method</edomvd>
            <edomvds>Neuendorf, K.K.E., Mehl, J.P., Jr., and Jackson, J.A., eds., 2011, Glossary of geology (5th ed., revised): Alexandria, Va., American Geosciences Institute, 783 p.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>CA-TIMS geochronology</edomv>
            <edomvd>Sample location of age dated rock using the chemical abrasion thermal ionization mass spectrometry (CA-TIMS) method (Mattison, 2005)</edomvd>
            <edomvds>Mattinson, J.M., 2005, Zircon U-Pb chemical abrasion ("CA–TIMS") method: combined annealing and multi-step dissolution analysis for improved precision and accuracy of zircon ages: Chemical Geology, v. 220, p. 47–66.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>LA-ICP-MS geochronology</edomv>
            <edomvd>Sample location of age dated rock using the laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS) method</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>FieldSampleID</attrlabl>
        <attrdef>Sample ID given at time of collection.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>AlternateSampleID</attrlabl>
        <attrdef>Museum #, lab #, etc.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>MapUnit</attrlabl>
        <attrdef>Short plain-text identifier of the map unit. Foreign key to DescriptionOfMapUnits table.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <edom>
            <edomv>Opv</edomv>
            <edomvd>Metafelsite volcanics and granofels member of the Partridge Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>MDp</edomv>
            <edomvd>Muscovite-biotite pegmatite of the New Hampshire Plutonic suite</edomvd>
            <edomvds>Bradley, D.C., Shea, E., Buchwaldt, R., Bowring, S., Benowitz, J., O’Sullivan, P., and McCauley, A., 2016, Geochronology and tectonic context of lithium-cesium-tantalum pegmatites in the Appalachians: Canadian Mineralogist, v. 54, no. 4, p. 945–969.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Oaf</edomv>
            <edomvd>Intermediate to felsic metatuff member of the Ammonoosuc Volcanics</edomvd>
            <edomvds>BF24KNHVTDAS03 | BF24KNHVTDAS15</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Sr</edomv>
            <edomvd>Schist and granofels member of the Rangeley Formation</edomvd>
            <edomvds>BF24KNHVTDAS14 | BF24KNHVTDAS07</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Dbg</edomv>
            <edomvd>Bethlehem Granodiorite of the New Hampshire Plutonic Suite</edomvd>
            <edomvds>BF24KNHVTDAS03 | BF24KNHVTDAS07 | BF24KNHVTDAS08</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Oog</edomv>
            <edomvd>Granite gneiss of the Alstead dome</edomvd>
            <edomvds>BF24KNHVTDAS04 | BF24KNHVTDAS15</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Opa</edomv>
            <edomvd>Amphibolite member of the Partridge Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Op</edomv>
            <edomvd>Rusty schist and granofels member of the Partridge Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Dl</edomv>
            <edomvd>Littleton Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Oot</edomv>
            <edomvd>Trondhjemite gneiss of the Alstead dome</edomvd>
            <edomvds>BF24KNHVTDAS03 | BF24KNHVTDAS15</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Srq</edomv>
            <edomvd>Quartzite, calc-silicate, and schist member of the Rangeley Formation</edomvd>
            <edomvds>BF24KNHVTDAS14 | BF24KNHVTDAS07</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Oaa</edomv>
            <edomvd>Amphibolite member of the Ammonoosuc Volcanics</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Symbol</attrlabl>
        <attrdef>Reference to a point marker, line symbol, or area-fill symbol that is used on the map graphic to denote the feature: perhaps a star for a K-Ar age locality, or a heavy black line for a fault.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Label</attrlabl>
        <attrdef>Plain-text equivalent of the desired annotation for a feature: for example "14 Ma", or "^c" which (when used with the FGDC GeoAge font) results in the geologic map-unit label TRc (with TR run together to make the Triassic symbol).</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>LocationConfidenceMeters</attrlabl>
        <attrdef>Estimated half-width in meters of positional uncertainty envelope; position is relative to other features in database.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Positive real number. Value of -9, -99, or -999 indicates value is unknown.</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>PlotAtScale</attrlabl>
        <attrdef>At what scale (or larger) should this observation or analysis be plotted? At smaller scales, it should not be plotted. Useful to prevent crowding of display at small scales and to display progressively more data at larger and larger scales. Value is scale denominator.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Positive real number.</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>MaterialAnalyzed</attrlabl>
        <attrdef>Earth-material which was analyzed, e.g., wood, shell, zircon, basalt, whole-rock.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>NumericAge</attrlabl>
        <attrdef>Age of map unit as shown in Description of Map Units. Examples of values are "late Holocene", "Pliocene and Miocene", "Lower Cretaceous".</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>AgePlusError</attrlabl>
        <attrdef>Positive (older) age error, measured in AgeUnits. Type of error (RMSE, 1 sigma, 2 sigma, 95% confidence limit) should be stated in Notes field.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Positive real number. Value of -9, -99, or -999 indicates value is unknown.</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>AgeMinusError</attrlabl>
        <attrdef>Negative (younger) age error, measured in AgeUnits. Type of error (RMSE, 1 sigma, 2 sigma, 95% confidence limit) should be stated in Notes field.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Positive real number. Value of -9, -99, or -999 indicates value is unknown.</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>AgeUnits</attrlabl>
        <attrdef>Units for NumericAge, AgePlusError, AgeMinusError.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <edom>
            <edomv>Ma</edomv>
            <edomvd>Mega-annum; millions of years before present</edomvd>
            <edomvds>Neuendorf, K.K.E., Mehl, J.P., Jr., and Jackson, J.A., eds., 2011, Glossary of geology (5th ed., revised): Alexandria, Va., American Geosciences Institute, 783 p.</edomvds>
          </edom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>StationsID</attrlabl>
        <attrdef>Foreign key to Stations point feature class.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>LocationSourceID</attrlabl>
        <attrdef>Source of location; foreign key to table DataSources.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <edom>
            <edomv>BF24KNHVTDAS03 | BF24KNHVTDAS07</edomv>
            <edomvd>BF24KNHVTDAS03 | BF24KNHVTDAS07</edomvd>
            <edomvds>This report</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>BF24KNHVTDAS03 | BF24KNHVTDAS15</edomv>
            <edomvd>BF24KNHVTDAS03 | BF24KNHVTDAS15</edomvd>
            <edomvds>This report</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>BF24KNHVTDAS04 | BF24KNHVTDAS15</edomv>
            <edomvd>BF24KNHVTDAS04 | BF24KNHVTDAS15</edomvd>
            <edomvds>This report</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>BF24KNHVTDAS14 | BF24KNHVTDAS07</edomv>
            <edomvd>BF24KNHVTDAS14 | BF24KNHVTDAS07</edomvd>
            <edomvds>This report</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>BF24KNHVTDAS04 | BF24KNHVTDAS14 | BF24KNHVTDAS16</edomv>
            <edomvd>BF24KNHVTDAS04 | BF24KNHVTDAS14 | BF24KNHVTDAS16</edomvd>
            <edomvds>This report</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>BF24KNHVTDAS14 | BF24KNHVTDAS07 | BF24KNHVTDAS04</edomv>
            <edomvd>BF24KNHVTDAS14 | BF24KNHVTDAS07 | BF24KNHVTDAS04</edomvd>
            <edomvds>This report</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>BF24KNHVTDAS05</edomv>
            <edomvd>Bradley, D.C., Shea, E., Buchwaldt, R., Bowring, S., Benowitz, J., O’Sullivan, P., and McCauley, A., 2016, Geochronology and tectonic context of lithium-cesium-tantalum pegmatites in the Appalachians: Canadian Mineralogist, v. 54, no. 4, p. 945–969.</edomvd>
            <edomvds>This report</edomvds>
          </edom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>AnalysisSourceID</attrlabl>
        <attrdef>Source of analysis; foreign key to table DataSources.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <edom>
            <edomv>BF24KNHVTDAS03 | BF24KNHVTDAS07</edomv>
            <edomvd>BF24KNHVTDAS03 | BF24KNHVTDAS07</edomvd>
            <edomvds>This report</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>BF24KNHVTDAS03 | BF24KNHVTDAS15</edomv>
            <edomvd>BF24KNHVTDAS03 | BF24KNHVTDAS15</edomvd>
            <edomvds>This report</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>BF24KNHVTDAS04 | BF24KNHVTDAS15</edomv>
            <edomvd>BF24KNHVTDAS04 | BF24KNHVTDAS15</edomvd>
            <edomvds>This report</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>BF24KNHVTDAS14 | BF24KNHVTDAS07</edomv>
            <edomvd>BF24KNHVTDAS14 | BF24KNHVTDAS07</edomvd>
            <edomvds>This report</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>BF24KNHVTDAS04 | BF24KNHVTDAS14 | BF24KNHVTDAS16</edomv>
            <edomvd>BF24KNHVTDAS04 | BF24KNHVTDAS14 | BF24KNHVTDAS16</edomvd>
            <edomvds>This report</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>BF24KNHVTDAS14 | BF24KNHVTDAS07 | BF24KNHVTDAS04</edomv>
            <edomvd>BF24KNHVTDAS14 | BF24KNHVTDAS07 | BF24KNHVTDAS04</edomvd>
            <edomvds>This report</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>BF24KNHVTDAS05</edomv>
            <edomvd>Bradley, D.C., Shea, E., Buchwaldt, R., Bowring, S., Benowitz, J., O’Sullivan, P., and McCauley, A., 2016, Geochronology and tectonic context of lithium-cesium-tantalum pegmatites in the Appalachians: Canadian Mineralogist, v. 54, no. 4, p. 945–969.</edomvd>
            <edomvds>This report</edomvds>
          </edom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Notes</attrlabl>
        <attrdef>Additional information specific to a particular feature or table entry.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain. Free text. Values of &lt;null&gt; or #null indicate no entry.</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>GeochronPoints_ID</attrlabl>
        <attrdef>Primary key.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Arbitrary string. Values should be unique within this database.</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>ErrorMeasure</attrlabl>
        <attrdef>Measure of error whose values are recorded in AgePlusError and AgeMinusError fields. Examples of values are "RMSE", "1 sigma", "2 sigma", "95% confidence interval."</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
    </detailed>
    <detailed>
      <enttyp>
        <enttypl>Stations</enttypl>
        <enttypd>Point locations of field observations and (or) samples. In the original file geodatabase, this dataset is found within the GeologicMap feature dataset.</enttypd>
        <enttypds>GeMS</enttypds>
      </enttyp>
      <attr>
        <attrlabl>OBJECTID</attrlabl>
        <attrdef>Internal feature number</attrdef>
        <attrdefs>ESRI</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Shape</attrlabl>
        <attrdef>Internal geometry object</attrdef>
        <attrdefs>ESRI</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>FieldID</attrlabl>
        <attrdef>Station number assigned by person who 
originally located this station. Commonly, 
key to field sheet and (or) field notebook.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>LocationConfidenceMeters</attrlabl>
        <attrdef>Estimated half-width in meters of positional uncertainty envelope; position is relative to other features in database.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Positive real number. Value of -9, -99, or -999 indicates value is unknown.</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>ObservedMapUnit</attrlabl>
        <attrdef>Short plain-text identifier of the map unit. Foreign key to DescriptionOfMapUnits table.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>MapUnit</attrlabl>
        <attrdef>Short plain-text identifier of the map unit. Foreign key to DescriptionOfMapUnits table.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <edom>
            <edomv>Dgqs</edomv>
            <edomvd>Gray quartzite and metapelite member of the Gile Mountain Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Ops</edomv>
            <edomvd>Pelitic schist and granofels member of the Partridge Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>DSwg</edomv>
            <edomvd>Large-garnet and hornblende garbenscheifer schist member of the Waits River Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Sr</edomv>
            <edomvd>Schist and granofels member of the Rangeley Formation</edomvd>
            <edomvds>BF24KNHVTDAS14 | BF24KNHVTDAS07</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Dbg</edomv>
            <edomvd>Bethlehem Granodiorite of the New Hampshire Plutonic Suite</edomvd>
            <edomvds>BF24KNHVTDAS03 | BF24KNHVTDAS07 | BF24KNHVTDAS08</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>DSws</edomv>
            <edomvd>Gray phyllite and schist member of the Waits River Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>DSwl</edomv>
            <edomvd>Limestone and schist member of the Waits River Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Scq</edomv>
            <edomvd>Quartzite and metaconglomerate member of the Clough Quartzite</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>DSwv</edomv>
            <edomvd>Laminated schist and granofels member of the Waits River Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Dg</edomv>
            <edomvd>Granite dikes of the New Hampshire Plutonic Suite</edomvd>
            <edomvds>Ratcliffe, N.M., Stanley, R.S., Gale, M.H., Thompson, P.J., and Walsh, G.J., 2011, Bedrock geologic map of Vermont: U.S. Geological Survey Scientific Investigations Map 3184, 3 sheets, scale 1:100,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Dl</edomv>
            <edomvd>Littleton Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Srq</edomv>
            <edomvd>Quartzite, calc-silicate, and schist member of the Rangeley Formation</edomvd>
            <edomvds>BF24KNHVTDAS14 | BF24KNHVTDAS07</edomvds>
          </edom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Symbol</attrlabl>
        <attrdef>Reference to a point marker, line symbol, or area-fill symbol that is used on the map graphic to denote the feature: perhaps a star for a K-Ar age locality, or a heavy black line for a fault.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Label</attrlabl>
        <attrdef>Plain-text equivalent of the desired annotation for a feature: for example "14 Ma", or "^c" which (when used with the FGDC GeoAge font) results in the geologic map-unit label TRc (with TR run together to make the Triassic symbol).</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>PlotAtScale</attrlabl>
        <attrdef>At what scale (or larger) should this observation or analysis be plotted? At smaller scales, it should not be plotted. Useful to prevent crowding of display at small scales and to display progressively more data at larger and larger scales. Value is scale denominator.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Positive real number.</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>DataSourceID</attrlabl>
        <attrdef>Source of data; foreign key to table DataSources.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <edom>
            <edomv>BF24KNHVTDAS01</edomv>
            <edomvd>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvd>
            <edomvds>This report</edomvds>
          </edom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Notes</attrlabl>
        <attrdef>Additional information specific to a particular feature or table entry.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain. Free text. Values of &lt;null&gt; or #null indicate no entry.</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>LocationMethod</attrlabl>
        <attrdef>Technique used to determine this station location Examples of values are "recreational GPS", "survey grade GPS", "by inspection", "by offset."</attrdef>
        <attrdefs>MISSING</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>TimeDate</attrlabl>
        <attrdef>Time and date of observation at station.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Observer</attrlabl>
        <attrdef>Name and affiliation of person who located this station. Example of value is "A.B. Geolog, UC Berkeley."</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>SignificantDimensionMeters</attrlabl>
        <attrdef>Significant dimension of exposure (in meters) at this station. Values could be thickness of stratigraphic section or depth of auger hole.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>GPSX</attrlabl>
        <attrdef>Measured GPS coordinate (easting). May differ from map coordinate because of GPS error or (more likely) base map error.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>GPSY</attrlabl>
        <attrdef>Measured GPS coordinate (northing). May differ from map coordinate because of GPS error or (more likely) base map error.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>PDOP</attrlabl>
        <attrdef>PDOP = Position Dilution Of Precision at this station; estimator of GPS accuracy. Null values permitted'</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>MapX</attrlabl>
        <attrdef>Station coordinate (easting) as compiled on the base map; base map should be identified in the DataSources record.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>MapY</attrlabl>
        <attrdef>Station coordinate (northing) as compiled on the base map; base map should be identified in the DataSources record.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Stations_ID</attrlabl>
        <attrdef>Primary key.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Arbitrary string. Values should be unique within this database.</udom>
        </attrdomv>
      </attr>
    </detailed>
    <detailed>
      <enttyp>
        <enttypl>GenericPoints</enttypl>
        <enttypd>Point feature class containing to locations of mineral resources from active or abandoned mines,  quarries or prospects.. May also contain the location of springs and other point features  In the original file geodatabase, this dataset is found within the GeologicMap feature dataset.</enttypd>
        <enttypds>BF24KNHVTDAS01</enttypds>
      </enttyp>
      <attr>
        <attrlabl>OBJECTID</attrlabl>
        <attrdef>Internal feature number</attrdef>
        <attrdefs>ESRI</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Shape</attrlabl>
        <attrdef>Internal geometry object</attrdef>
        <attrdefs>ESRI</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Type</attrlabl>
        <attrdef>Classifier that specifies what kind of geologic feature is represented by a database element: that a certain line within feature class ContactsAndFaults is a contact, or thrust fault, or water boundary; or that a point in GeochronPoints represents a K-Ar date.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <edom>
            <edomv>spring</edomv>
            <edomvd>The location where groundwater flows naturally from a rock or the soil onto the land surface or into a body of surface water</edomvd>
            <edomvds>Neuendorf, K.K.E., Mehl, J.P., Jr., and Jackson, J.A., eds., 2011, Glossary of geology (5th ed., revised): Alexandria, Va., American Geosciences Institute, 783 p.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>abandoned mine, prospect, or occurrence</edomv>
            <edomvd>The location of abandoned aboveground and (or) underground excavation for the extraction of mineral deposits or dimension stone or an area that was a potential site of mineral deposits, based on preliminary exploration</edomvd>
            <edomvds>Neuendorf, K.K.E., Mehl, J.P., Jr., and Jackson, J.A., eds., 2011, Glossary of geology (5th ed., revised): Alexandria, Va., American Geosciences Institute, 783 p.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>quarry</edomv>
            <edomvd>The location of the extraction or previous extraction of building stone or other valuable nonmetallic constituent from a surface mine</edomvd>
            <edomvds>Neuendorf, K.K.E., Mehl, J.P., Jr., and Jackson, J.A., eds., 2011, Glossary of geology (5th ed., revised): Alexandria, Va., American Geosciences Institute, 783 p.</edomvds>
          </edom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Symbol</attrlabl>
        <attrdef>Reference to a point marker, line symbol, or area-fill symbol that is used on the map graphic to denote the feature: perhaps a star for a K-Ar age locality, or a heavy black line for a fault.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Label</attrlabl>
        <attrdef>Plain-text equivalent of the desired annotation for a feature: for example "14 Ma", or "^c" which (when used with the FGDC GeoAge font) results in the geologic map-unit label TRc (with TR run together to make the Triassic symbol).</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>LocationConfidenceMeters</attrlabl>
        <attrdef>Estimated half-width in meters of positional uncertainty envelope; position is relative to other features in database.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Positive real number. Value of -9, -99, or -999 indicates value is unknown.</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>PlotAtScale</attrlabl>
        <attrdef>At what scale (or larger) should this observation or analysis be plotted? At smaller scales, it should not be plotted. Useful to prevent crowding of display at small scales and to display progressively more data at larger and larger scales. Value is scale denominator.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Positive real number.</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>StationsID</attrlabl>
        <attrdef>Foreign key to Stations point feature class.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>MapUnit</attrlabl>
        <attrdef>Short plain-text identifier of the map unit. Foreign key to DescriptionOfMapUnits table.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <edom>
            <edomv>Dgqs</edomv>
            <edomvd>Gray quartzite and metapelite member of the Gile Mountain Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>MDp</edomv>
            <edomvd>Muscovite-biotite pegmatite of the New Hampshire Plutonic suite</edomvd>
            <edomvds>Bradley, D.C., Shea, E., Buchwaldt, R., Bowring, S., Benowitz, J., O’Sullivan, P., and McCauley, A., 2016, Geochronology and tectonic context of lithium-cesium-tantalum pegmatites in the Appalachians: Canadian Mineralogist, v. 54, no. 4, p. 945–969.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>DSwsv</edomv>
            <edomvd>Metavolcaniclastic members of the Waits River Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Dbg</edomv>
            <edomvd>Bethlehem Granodiorite of the New Hampshire Plutonic Suite</edomvd>
            <edomvds>BF24KNHVTDAS03 | BF24KNHVTDAS07 | BF24KNHVTDAS08</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>DSwv</edomv>
            <edomvd>Laminated schist and granofels member of the Waits River Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Scq</edomv>
            <edomvd>Quartzite and metaconglomerate member of the Clough Quartzite</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Op</edomv>
            <edomvd>Rusty schist and granofels member of the Partridge Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Dl</edomv>
            <edomvd>Littleton Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>DSwa</edomv>
            <edomvd>Amphibolite and greenstone member of the Waits River Formation</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Oot</edomv>
            <edomvd>Trondhjemite gneiss of the Alstead dome</edomvd>
            <edomvds>BF24KNHVTDAS03 | BF24KNHVTDAS15</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Oaa</edomv>
            <edomvd>Amphibolite member of the Ammonoosuc Volcanics</edomvd>
            <edomvds>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvds>
          </edom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>LocationSourceID</attrlabl>
        <attrdef>Source of location; foreign key to table DataSources.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <edom>
            <edomv>BF24KNHVTDAS01</edomv>
            <edomvd>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvd>
            <edomvds>This report</edomvds>
          </edom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>DataSourceID</attrlabl>
        <attrdef>Source of data; foreign key to table DataSources.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <edom>
            <edomv>BF24KNHVTDAS01</edomv>
            <edomvd>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000.</edomvd>
            <edomvds>This report</edomvds>
          </edom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Notes</attrlabl>
        <attrdef>Additional information specific to a particular feature or table entry. Notes in this feature class contain URLs for the MRDS entry of the feature if it's available.</attrdef>
        <attrdefs>BF24KNHVTDAS01</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain. Free text. Values of &lt;null&gt; or #null indicate no entry.</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>GenericPoints_ID</attrlabl>
        <attrdef>Primary key.</attrdef>
        <attrdefs>GeMS</attrdefs>
        <attrdomv>
          <udom>Arbitrary string. Values should be unique within this database.</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>MineLabel</attrlabl>
        <attrdef>Label of the mine as defined on published geologic map. Information most likely from the MRDS (Mineral Resources Data System).</attrdef>
        <attrdefs>BF24KNHVTDAS01</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Material</attrlabl>
        <attrdef>Material being mined or quarried; valid entries are abbreviations of minerals or building material common to the mining and (or) construction industries. Users of this database should consult with table 1 on the published geologic map of this product.</attrdef>
        <attrdefs>BF24KNHVTDAS01</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
    </detailed>
    <detailed>
      <enttyp>
        <enttypl>GeologicMapAnno</enttypl>
        <enttypd>ArcGIS annotation feature class. This annotation feature class does not contain labels for folds or faults. In the original file geodatabase, this dataset is found within the GeologicMap feature dataset.</enttypd>
        <enttypds>ESRI</enttypds>
      </enttyp>
      <attr>
        <attrlabl>OBJECTID</attrlabl>
        <attrdef>Internal feature number</attrdef>
        <attrdefs>ESRI</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Shape</attrlabl>
        <attrdef>Internal geometry object</attrdef>
        <attrdefs>ESRI</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>FeatureID</attrlabl>
        <attrdef>Value controls placement or representation of annotation</attrdef>
        <attrdefs>ESRI</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>ZOrder</attrlabl>
        <attrdef>Value controls placement or representation of annotation</attrdef>
        <attrdefs>ESRI</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>AnnotationClassID</attrlabl>
        <attrdef>Value controls placement or representation of annotation</attrdef>
        <attrdefs>ESRI</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Element</attrlabl>
        <attrdef>Value controls placement or representation of annotation</attrdef>
        <attrdefs>ESRI</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>SymbolID</attrlabl>
        <attrdef>Value controls placement or representation of annotation</attrdef>
        <attrdefs>ESRI</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Status</attrlabl>
        <attrdef>Value controls placement or representation of annotation</attrdef>
        <attrdefs>ESRI</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>TextString</attrlabl>
        <attrdef>Value controls placement or representation of annotation</attrdef>
        <attrdefs>ESRI</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>FontName</attrlabl>
        <attrdef>Value controls placement or representation of annotation</attrdef>
        <attrdefs>ESRI</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>FontStyle</attrlabl>
        <attrdef>Value controls placement or representation of annotation</attrdef>
        <attrdefs>ESRI</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>FontSize</attrlabl>
        <attrdef>Value controls placement or representation of annotation</attrdef>
        <attrdefs>ESRI</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Underline</attrlabl>
        <attrdef>Value controls placement or representation of annotation</attrdef>
        <attrdefs>ESRI</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>VerticalAlignment</attrlabl>
        <attrdef>Value controls placement or representation of annotation</attrdef>
        <attrdefs>ESRI</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>HorizontalAlignment</attrlabl>
        <attrdef>Value controls placement or representation of annotation</attrdef>
        <attrdefs>ESRI</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>XOffset</attrlabl>
        <attrdef>Value controls placement or representation of annotation</attrdef>
        <attrdefs>ESRI</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>YOffset</attrlabl>
        <attrdef>Value controls placement or representation of annotation</attrdef>
        <attrdefs>ESRI</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Angle</attrlabl>
        <attrdef>Value controls placement or representation of annotation</attrdef>
        <attrdefs>ESRI</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>FontLeading</attrlabl>
        <attrdef>Value controls placement or representation of annotation</attrdef>
        <attrdefs>ESRI</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>WordSpacing</attrlabl>
        <attrdef>Value controls placement or representation of annotation</attrdef>
        <attrdefs>ESRI</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>CharacterWidth</attrlabl>
        <attrdef>Value controls placement or representation of annotation</attrdef>
        <attrdefs>ESRI</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>CharacterSpacing</attrlabl>
        <attrdef>Value controls placement or representation of annotation</attrdef>
        <attrdefs>ESRI</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>FlipAngle</attrlabl>
        <attrdef>Value controls placement or representation of annotation</attrdef>
        <attrdefs>ESRI</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Shape_Length</attrlabl>
        <attrdef>Internal feature length, double</attrdef>
        <attrdefs>ESRI</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>Shape_Area</attrlabl>
        <attrdef>Internal feature area, double</attrdef>
        <attrdefs>ESRI</attrdefs>
        <attrdomv>
          <udom>Unrepresentable domain</udom>
        </attrdomv>
      </attr>
    </detailed>
    <overview>
      <eaover>The geodatabase contains the following elements: non-spatial table Glossary (65 rows); non-spatial table DataSources (21 rows); non-spatial table DescriptionOfMapUnits (63 rows); non-spatial table GeoMaterialDict (101 rows); feature dataset GeologicMap which contains feature class MapUnitPolys (214 features), feature class OverlayPolys (1814 features), feature class ContactsAndFaults (432 features), feature class GeologicLines (32 features), feature class CartographicLines (2 features), feature class GeochronPoints (16 features), feature class GenericPoints (31 features), feature class OrientationPoints (6111 features), feature class Stations (33 features), feature class GeologicMapAnno (3641 features)</eaover>
      <eadetcit>Merschat, A.J., Walsh, G.J., Valley, P.M., McAleer, R.J., and Armstrong, T.R., 2025, Bedrock geologic map of the Bellows Falls 7.5- x 15-minute quadrangle, Windham and Windsor Counties, Vermont, and Sullivan and Cheshire Counties, New Hampshire: U.S. Geological Survey Scientific Investigations Map 3535, 2 sheets, scale 1:24,000, https://doi.org/10.3133/sim3535</eadetcit>
    </overview>
  </eainfo>
  <distinfo>
    <distrib>
      <cntinfo>
        <cntorgp>
          <cntorg>U.S. Geological Survey</cntorg>
          <cntper>GS ScienceBase</cntper>
        </cntorgp>
        <cntaddr>
          <addrtype>mailing</addrtype>
          <address>Denver Federal Center, Building 810, Mail Stop 302</address>
          <city>Denver</city>
          <state>CO</state>
          <postal>80225</postal>
          <country>US</country>
        </cntaddr>
        <cntvoice>1-888-275-8747</cntvoice>
        <cntemail>sciencebase@usgs.gov</cntemail>
      </cntinfo>
    </distrib>
    <distliab>Unless otherwise stated, all data, metadata and related materials are considered to satisfy the quality standards relative to the purpose for which the data were collected. Although these data and associated metadata have been reviewed for accuracy and completeness and approved for release by the U.S. Geological Survey (USGS), no warranty expressed or implied is made regarding the display or utility of the data on any other system or for general or scientific purposes, nor shall the act of distribution constitute any such warranty. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government.</distliab>
    <stdorder>
      <digform>
        <digtinfo>
          <formname>Digital Data</formname>
        </digtinfo>
        <digtopt>
          <onlinopt>
            <computer>
              <networka>
                <networkr>https://doi.org/10.5066/P172BBFC</networkr>
              </networka>
            </computer>
          </onlinopt>
        </digtopt>
      </digform>
      <fees>None</fees>
    </stdorder>
  </distinfo>
  <metainfo>
    <metd>20250521</metd>
    <metc>
      <cntinfo>
        <cntorgp>
          <cntorg>U.S. Geological Survey, Northeast Region</cntorg>
          <cntper>Ernest A Crider</cntper>
        </cntorgp>
        <cntpos>Geologist</cntpos>
        <cntaddr>
          <addrtype>mailing</addrtype>
          <address>Mail Stop 926A, 12201 Sunrise Valley Dr</address>
          <city>Reston</city>
          <state>VA</state>
          <postal>20192</postal>
          <country>US</country>
        </cntaddr>
        <cntvoice>703-648-6906</cntvoice>
        <cntfax>703-648-6953</cntfax>
        <cntemail>ecrider@usgs.gov</cntemail>
      </cntinfo>
    </metc>
    <metstdn>FGDC Content Standard for Digital Geospatial Metadata</metstdn>
    <metstdv>FGDC-STD-001-1998</metstdv>
    <mettc>local time</mettc>
  </metainfo>
</metadata>
