Lay Dam Formation is named in this report and subdivided into Kalona Quartzite Member and overlying Miller Mill Quartzite Member. Miller Mill consists of medium- to coarse-grained, locally conglomeratic quartzite. Reaches a maximum of 950 ft in thickness. Underlies Butting Ram Sandstone. Age is Early Devonian.
Source: GNU records (USGS DDS-6; Reston GNULEX).
Miller Mill Quartzite Member of Lay Dam Formation is a white to medium-gray medium- to coarse-grained, quartzose to feldspathic quartzite, with local conglomeratic zones. Occurs in the northern Piedmont of AL. Underlies the Erin Slate Member; overlies Heflin Phyllite. Age is Silurian(?) to Devonian(?).
Source: GNU records (USGS DDS-6; Reston GNULEX).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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