Informal name Oak formation proposed to replace a variety of common names (residual material, weathered bedrock, paleosol geest, clay, and pedisediment) used for the pre-Illinoian deposits that underlie the Glasford Formation, the Teneriffe Silt, or the Loveland Silt in the study area. Oak formation is a residuum, a product mainly of in situ weathering, and has attributes of both a soil and a lithologic unit. It is laterally continuous in the study area and has lithologic properties distinctly different from those of the underlying indurated bedrock.
Source: GNU records (USGS DDS-6; Reston GNULEX).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
Asterisk (*) indicates published by U.S. Geological Survey authors.
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