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Lava complex at the Sarvent Glaciers. Basaltic andesite lava flows and intercalated volcanic clastic rocks of the Ohanapecosh Formation dip gently westward. The prominent planar surface was formed by erosion of softer Ohanapecosh volcanic clastic rocks lying above the thick sequence of lava flows. Mount Rainier National Park, Washington. ca. 1959. Figure 3, U.S. Geological Survey Professional paper 444.


    map background search result map search result map Lava complex at the Sarvent Glaciers. Mount Rainier National Park, Washington. ca. 1959. Lava complex at the Sarvent Glaciers. Mount Rainier National Park, Washington. ca. 1959.