[Probably] named for exposures in Bernice Canyon, T22N R37E, Clan Alpine Mountains, Churchill Co., NV. [Type locality not designated.] Consists of mudstone with minor wacke, quartz arenite, and limestone. Is 2,600 m thick. Overlies Triassic pelite; conformably underlies Hoyt Canyon Formation. Is Late Triassic age.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
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