Mapped in Lincoln Co, NV, Great Basin province; exposed in southwest quarter of quad. Redescribed; lower 60 m consists of light-gray, coarse-grained, massive dolomite and upper 60 m consists of dark gray, coarse-grained, thick-bedded to massive, locally cherty dolomite that is commonly mottled, and includes "tiger-stripped" zones of secondary dolomitization. Lower part is incompletely exposed. Nopah is commonly tectonically brecciated; breccia is recemented forming resistant ledges and cliffs. No fossils found in this quad though silicified brachiopods EOORTHIS sp. found in adjacent Lime Mountain quad. Unit is about 120 m thick. Nopah is oldest exposed unit; conformably underlies lower part of Pogonip Group. Late Cambrian age.
Source: GNU records (USGS DDS-6; Denver GNULEX).
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