Unit is named the Shellrock Point Volcanics. Is exposed on Pogue Mountain and Pogue Flat in the Okanogan Range, WA. Consists of quartz keratophyre flows containing medium-grained phenocrysts of quartz and pink albite in a dense white to pale-green groundmass. May be older than the Miocene Columbia River Basalt [Group]; may correlate with early Tertiary keratophyre flows to the north. (B1565)
Source: GNU records (USGS DDS-6; Menlo GNULEX).
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