Named as a member of Plateau Rhyolite (new) for exposures in Upper Geyser Basin (its type area), west-central Yellowstone National Park, WY in Yellowstone province. Includes early postcaldera rhyolitic lava flows and associated pyroclastic deposits that were erupted within the Yellowstone caldera after doming. Is characterized by abundant plagioclase phenocrysts, commonly oligoclase that is highly embayed. Is exposed only in upper Grand Canyon and area southeast to Fern Lake. Is younger than Mallard Lake Member (new) of Plateau Rhyolite. Is older than Central Plateau Member (new) of Plateau Rhyolite. K-Ar dating of sanidine, plagioclase, and nonhydrated glass from rhyolites shows most of the flows are younger than Lava Creek Tuff (new). Is part of the third volcanic cycle of Yellowstone Plateau. Cross sections; stratigraphic table.
Source: GNU records (USGS DDS-6; Denver GNULEX).
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