<?xml version='1.0' encoding='UTF-8'?>
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  <idinfo>
    <citation>
      <citeinfo>
        <origin>Petersen, Mark D.</origin>
        <origin>Harmsen, Stephen C.</origin>
        <origin>Jaiswal, Kishor S.</origin>
        <origin>Rukstales, Kenneth S.</origin>
        <origin>Luco, Nicolas</origin>
        <origin>Haller, Kathleen M.</origin>
        <origin>Mueller, Charles S.</origin>
        <origin>Shumway, Allison M.</origin>
        <pubdate>2018</pubdate>
        <title>2k) Probabilistic seismic hazard maps and data for South America: Modified Mercalli Intensity, based on peak ground acceleration, with a 2% probability of exceedance in 50 years</title>
        <geoform>GEOTIFF</geoform>
        <othercit>Digital geospatial data and supporting metadata can be downloaded from:
https://doi.org/10.5066/F7WM1BK1</othercit>
        <onlink>https://doi.org/10.5066/F7WM1BK1</onlink>
        <lworkcit>
          <citeinfo>
            <origin>Petersen, Mark D.</origin>
            <origin>Harmsen, Stephen C.</origin>
            <origin>Jaiswal, Kishor S.</origin>
            <origin>Rukstales, Kenneth S.</origin>
            <origin>Luco, Nicolas</origin>
            <origin>Haller, Kathleen M.</origin>
            <origin>Mueller, Charles S.</origin>
            <origin>Shumway, Allison M.</origin>
            <pubdate>20180116</pubdate>
            <title>Seismic Hazard, Risk, and Design for South America</title>
            <geoform>publication</geoform>
            <serinfo>
              <sername>Bulletin of the Seismological Society of America</sername>
              <issue>doi:  10.1785/0120170002</issue>
            </serinfo>
            <pubinfo>
              <pubplace>Albany, CA</pubplace>
              <publish>Seismological Society of America</publish>
            </pubinfo>
            <onlink>https://doi.org/10.1785/0120170002</onlink>
          </citeinfo>
        </lworkcit>
      </citeinfo>
    </citation>
    <descript>
      <abstract>A seismic hazard model for South America, based on a smoothed (gridded) seismicity model, a subduction model, a crustal fault model, and a ground motion model, has been produced by the U.S. Geological Survey.  These models are combined to account for ground shaking from earthquakes on known faults as well as earthquakes on un-modeled faults.
This data set represents the results of calculations of hazard curves for a grid of points with a spacing of 0.1 degrees in latitude and longitude.  It represents Modified Mercalli Intensity (MMI) with a 10% probability of exceedance in 50 year.  The maps and data were derived from PGA ground-motion conversions of Worden et al. (2012), and include soil amplification based on a topographic proxy of Allen and Wald (2009), and site amplification based on Seyhan and Stewart (2014) relationships.</abstract>
      <purpose>This map is intended to provide an estimate of Modified Mercalli Intensity (MMI) with a 10% probability of exceedance in 50 years.</purpose>
    </descript>
    <timeperd>
      <timeinfo>
        <sngdate>
          <caldate>2017</caldate>
        </sngdate>
      </timeinfo>
      <current>publication date</current>
    </timeperd>
    <status>
      <progress>Complete</progress>
      <update>None planned</update>
    </status>
    <spdom>
      <bounding>
        <westbc>-85.05</westbc>
        <eastbc>-19.95</eastbc>
        <northbc>15.05</northbc>
        <southbc>-70.05</southbc>
      </bounding>
    </spdom>
    <keywords>
      <theme>
        <themekt>none</themekt>
        <themekey>Seismic</themekey>
        <themekey>Earthquake</themekey>
        <themekey>Hazard</themekey>
        <themekey>Risk</themekey>
      </theme>
      <theme>
        <themekt>USGS Metadata Identifier</themekt>
        <themekey>USGS:59c9840ee4b017cf313f1146</themekey>
      </theme>
      <place>
        <placekt>http://geonames.usgs.gov/</placekt>
        <placekey>Argentina</placekey>
        <placekey>Bolivia</placekey>
        <placekey>Brazil</placekey>
        <placekey>Chile</placekey>
        <placekey>Colombia</placekey>
        <placekey>Ecuador</placekey>
        <placekey>French Guiana</placekey>
        <placekey>Guyana</placekey>
        <placekey>Panama</placekey>
        <placekey>Paraguay</placekey>
        <placekey>Peru</placekey>
        <placekey>Suriname</placekey>
        <placekey>Trinidad and Tobago</placekey>
        <placekey>Uruguay</placekey>
        <placekey>Venezuela</placekey>
        <placekey>South America</placekey>
      </place>
      <temporal>
        <tempkt>none</tempkt>
        <tempkey>2017</tempkey>
      </temporal>
    </keywords>
    <accconst>None</accconst>
    <useconst>Acknowledgment of  the U.S. Geological Survey, National Seismic Hazard Mapping Project would be appreciated in products derived from these data.</useconst>
    <ptcontac>
      <cntinfo>
        <cntperp>
          <cntper>Ken Rukstales</cntper>
          <cntorg>U.S. Geological Survey - Geologic Hazards Science Center</cntorg>
        </cntperp>
        <cntaddr>
          <addrtype>mailing address</addrtype>
          <address>Box 25046, MS 966</address>
          <city>Denver</city>
          <state>CO</state>
          <postal>80225</postal>
          <country>USA</country>
        </cntaddr>
        <cntvoice>303-273-8677</cntvoice>
        <cntemail>rukstales@usgs.gov</cntemail>
      </cntinfo>
    </ptcontac>
    <native>Microsoft Windows 7
Esri ArcGIS 10.3</native>
    <crossref>
      <citeinfo>
        <origin>Allen, T.I.</origin>
        <origin>Wald, D.J.</origin>
        <pubdate>2009</pubdate>
        <title>On the use of high-resolution topographic data as a proxy for seismic site conditions (VS30)</title>
        <geoform>publication</geoform>
        <serinfo>
          <sername>Bulletin of the Seismological Society of America</sername>
          <issue>v. 99, p. 935-943</issue>
        </serinfo>
      </citeinfo>
    </crossref>
    <crossref>
      <citeinfo>
        <origin>Seyhan, E.</origin>
        <origin>Stewart, J.P.</origin>
        <pubdate>2014</pubdate>
        <title>Semi-empirical nonlinear site amplification from NGA-West2 data and simulations</title>
        <geoform>publication</geoform>
        <serinfo>
          <sername>Earthquake Spectra</sername>
          <issue>v. 30, 1241-1256, doi:10.1193/063013EQS181M</issue>
        </serinfo>
      </citeinfo>
    </crossref>
    <crossref>
      <citeinfo>
        <origin>Worden, C.B.</origin>
        <origin>Gerstenberger, M.C.</origin>
        <origin>Rhoades, D.A.</origin>
        <origin>Wald, D.J.</origin>
        <pubdate>2012</pubdate>
        <title>Probabilistic relationships between ground-motion parameters and modified Mercalli intensity in California</title>
        <geoform>publication</geoform>
        <serinfo>
          <sername>Bulletin of the Seismological Society of America</sername>
          <issue>v. 102, p. 204-221</issue>
        </serinfo>
      </citeinfo>
    </crossref>
  </idinfo>
  <dataqual>
    <attracc>
      <attraccr>This data set is based on a seismological model.  The following report provides information on quality assessment for the data set:
Petersen, M.D., Harmsen, S.C., Jaiswal, K.S., Rukstales, K.S., Luco, Nicolas, Haller, K.M., Mueller, C.S., and Shumway, A.M., 2018, Seismic Hazard, Risk, and Design for South America:  Bulletin of the Seismological Society of America, doi:  10.1785/0120170002</attraccr>
    </attracc>
    <logic>Data have not been resampled.  All values are within the permissible range of the Modified Mercalli Intensity scale.</logic>
    <complete>Data outside the physical boundaries of South America and the study area have been assigned a NODATA value.</complete>
    <posacc>
      <horizpa>
        <horizpar>The location of features is based on calculations of a seismological model for the study area.  The location of each point is considered to be correct within the confines of computer accuracy.</horizpar>
      </horizpa>
    </posacc>
    <lineage>
      <procstep>
        <procdesc>Based upon the 2017 USGS Seismic Hazard Model for South America, a suite of hazard curves were calculated for an equally spaced grid of points covering the South America.  The grid has a cell spacing of 0.1 degrees in both latitude and longitude.   Using log-log interpolation, the hazard curves at each grid point were used to determine the peak ground accelerations that have an annual frequency of exceedance of 0.0021 (475 year return period) for each grid point.  Using the topographic-based soil classification methods of Wald and Allen (2009), the calculated ground motions were amplified for soil type based on the amplification factors of Stewart and Seyhan (2014).  Finally, the amplified ground motions for peak ground acceleration were converted to Modified Mercalli Intensities using the the relationships of Worden and others (2012).</procdesc>
        <procdate>2017</procdate>
      </procstep>
    </lineage>
  </dataqual>
  <spdoinfo>
    <direct>Raster</direct>
    <rastinfo>
      <rasttype>Pixel</rasttype>
      <rowcount>851</rowcount>
      <colcount>651</colcount>
    </rastinfo>
  </spdoinfo>
  <spref>
    <horizsys>
      <geograph>
        <latres>0.1</latres>
        <longres>0.1</longres>
        <geogunit>Decimal degrees</geogunit>
      </geograph>
      <geodetic>
        <horizdn>D_WGS_1984</horizdn>
        <ellips>World Geodetic System 1984</ellips>
        <semiaxis>6378137</semiaxis>
        <denflat>298.257223563</denflat>
      </geodetic>
    </horizsys>
  </spref>
  <eainfo>
    <detailed>
      <enttyp>
        <enttypl>SA_10PctIn50Yrs_MMI_Soils.tif</enttypl>
        <enttypd>Modified Mercalli Intensity based on peak ground acceleration, with 10% probability of exceedance in 50 years</enttypd>
        <enttypds>USGS</enttypds>
      </enttyp>
    </detailed>
    <overview>
      <eaover>Each pixel contains a decimal Modified Mercalli Intensity value that has a 10% probability of exceedance in fifty year.  For display purposes, the pixel values should be classified as follows:
Decimal MMI range                        MMI classification
------------------------------                        --------------------------
1.0 - 3.5                                          &lt;= III
3.5 - 4.5                                           IV
4.5 - 5.5                                           V
5.5 - 6.5                                           VI
6.5 - 7.5                                           VII
7.5 - 8.5                                           VIII
&gt; 8.5                                               &gt;= IX</eaover>
      <eadetcit>http://pubs.usgs.gov/gip/earthq4/severitygip.html</eadetcit>
    </overview>
  </eainfo>
  <distinfo>
    <distrib>
      <cntinfo>
        <cntorgp>
          <cntorg>U.S. Geological Survey - ScienceBase</cntorg>
        </cntorgp>
        <cntaddr>
          <addrtype>mailing address</addrtype>
          <address>Denver Federal Center, Building 810, Mail Stop 302</address>
          <city>Lakewood</city>
          <state>CO</state>
          <postal>80215</postal>
          <country>USA</country>
        </cntaddr>
        <cntvoice>1-888-275-8747</cntvoice>
        <cntemail>sciencebase@usgs.gov</cntemail>
      </cntinfo>
    </distrib>
    <resdesc>Downloadable raster data set in raster format.</resdesc>
    <distliab>Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this information product, for the most part, is in the public domain, it also contains copyrighted materials as noted in the text. Permission to reproduce copyrighted items must be secured from the copyright owner whenever applicable. The data have been approved for release and publication by the U.S. Geological Survey (USGS). Although the data have been subjected to rigorous review and are substantially complete, the USGS reserves the right to revise the data pursuant to further analysis and review. Furthermore, the data are released on the condition that neither the USGS nor the U.S. Government may be held liable for any damages resulting from authorized or unauthorized use. Although the data have been processed successfully on a computer system at the U.S. Geological Survey, 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. The U.S. Geological Survey shall not be held liable for improper or incorrect use of the data described and/or contained herein. Users of the data are advised to read all metadata and associated documentation thoroughly to understand appropriate use and data limitations.</distliab>
    <stdorder>
      <digform>
        <digtinfo>
          <formname>TIFF</formname>
          <formvern>42</formvern>
          <formspec>TIFF image with world file</formspec>
          <formcont>Modified Mercalli Intensity based on peak ground acceleration, with 10% probability of exceedance in 50 years</formcont>
          <filedec>Files need to be decompressed using winzip or similar utility</filedec>
          <transize>0.5</transize>
        </digtinfo>
        <digtopt>
          <onlinopt>
            <computer>
              <networka>
                <networkr>https://doi.org/10.5066/F7Wm1BK1</networkr>
              </networka>
            </computer>
          </onlinopt>
        </digtopt>
      </digform>
      <fees>none</fees>
    </stdorder>
  </distinfo>
  <metainfo>
    <metd>20260424</metd>
    <metc>
      <cntinfo>
        <cntorgp>
          <cntorg>U.S. Geological Survey - Geologic Hazards Science Center</cntorg>
          <cntper>Ken Rukstales</cntper>
        </cntorgp>
        <cntaddr>
          <addrtype>mailing address</addrtype>
          <address>Box 25046, MS 966</address>
          <city>Lakewood</city>
          <state>CO</state>
          <postal>80225</postal>
          <country>USA</country>
        </cntaddr>
        <cntvoice>303-273-8677</cntvoice>
        <cntemail>ghsc_metadata@usgs.gov</cntemail>
      </cntinfo>
    </metc>
    <metstdn>FGDC Content Standards for Digital Geospatial Metadata</metstdn>
    <metstdv>FGDC-STD-001-1998</metstdv>
    <mettc>local time</mettc>
  </metainfo>
</metadata>
