Pg. 7, 9 (stratigraphic column) [section by L.V. Rickard]. Forge Hollow member of Bertie formation. Gypsiferous shales, 25 to 40 feet thick. Overlies Fiddlers Green member; underlies Williamsville member. Age is Late Silurian.
[Type lcoality not stated.] Occurs in Clockville and Munnsville areas, central NY.
Source: US geologic names lexicon (USGS Bull. 1200, p. 1388-1389).
Forge Hollow dolomite of Bertie group. Rank raised to formation in Bertie group. Overlies Fiddlers Green dolomite; underlies Oxbow dolomite (new). Fieldwork has not demonstrated lateral continuity of Forge Hollow and Scajaquada as indicated on present chart. Thick glacial deposits conceal these units in area where they may merge. Possibility of facies changes -- for example, Falkirk to Forge Hollow -- should not be overlooked. For the present, the distinct names are retained for western and central New York.
Source: US geologic names lexicon (USGS Bull. 1200, p. 1388-1389).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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