An informal name mapped by Veatch (1907) and Walker (1950). Considered to be a syntectonic deposit that resulted from early movement on the Absaroka fault. Has some pollen types that also occur in the Bear River Formation. CHATANGIELLA Interval zone (marine) and PROTEACIDITES RETUSUS Interval Zone (nonmarine) contemporaneous palynomorph biozones. Assigned a Cenomanian age. Samples collected in Lincoln Co, WY in the Greater Green River basin.
Source: GNU records (USGS DDS-6; Denver GNULEX).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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