Unit is named the Windy Hill Quartz Dioritic Orthogneiss. Is a late synmetamorphic plutonic unit in the Okanogan Range, WA. Intrudes the Salmon Creek schists and gneisses; is intruded by the Late Cretaceous Conconully Granodiorite (new). Is of the same general age as the Leader Mountain Granodioritic Gneiss and the Reed Creek Quartz Dioritic Gneiss and is similar to them in mineralogy, texture, and structure. Age is Late Triassic or Early Jurassic. (B1565)
Source: GNU records (USGS DDS-6; Menlo GNULEX).
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