In the subsurface, the Pride Mountain contains two major mappable sandstone members, the Lewis and the Evans. The Evans undergoes a facies change in southeastern Monroe and northern Lowndes Cos., MS, and becomes the lowest resistive black shale unit of the Neal Black Shale. The Lewis is continuous across the entire northern shelf of the basin and does not undergo a downdip facies change. Johnson (1988) recognized four coarsening- and shallowing-upward siliciclastic "cycles." He correlated his first (oldest) cycle with the Lewis and his third cycle with the Evans.
Source: GNU records (USGS DDS-6; Reston GNULEX).
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