On May 18, 1980, Mount St. Helens, Washington, exploded in a spectacular and devastating eruption that resulted in previously unimaginable events that drastically altered the mountain and the surrounding area. One unprecedented event was the collapse of the summit and north flank of the volcano forming a huge landslide known as the ‘debris avalanche’ with a total volume of about 2.5 km3 (3.3 billion cubic yards). The debris avalanche swept around and up ridges to the north, but most of it turned westward as far as 23 km (14 mi) down the valley of the North Fork Toutle River and formed a hummocky deposit. This had a profound effect on the topography of the area, including transforming the summit cone of the volcano into an amphitheater-shaped crater, in places, burying the valley north of the volcano under hundreds of feet of debris, and filling the Spirit Lake basin raising the surface elevation 64 m (210 ft). This release consists of a 10-meter resolution digital elevation model, covering an area of 196.45 sq km, and hillshade map of the summit and valley north of the volcano circa 1952 surface derived from contour lines digitized from historic topographic maps. These data represent the paleo topography of Mt St. Helens and vicinity that were most significantly altered by the 1980 eruption and debris avalanche.