Named the Vintage dolomite for Vintage, Lancaster Co., southeastern PA. Consists of gray, heavy-bedded dolomite which weathers to whitish chalky surface, and knotty, dark-blue dolomite with argillaceous partings. Some beds are sparkling gray to blue mottled with siliceous and calcareous blebs that stand out on weathered surfaces. The base is a whitish, schistose, thin-bedded, impure dolomite containing muscovite flakes. Thickness is 500 to 650 feet. Overlies Antietam quartzite and underlies Kinzers formation. The Vintage is of Early Cambrian age.
Source: GNU records (USGS DDS-6; Reston GNULEX).
The Vintage Formation in the Lebanon Valley sequence of eastern PA consists of dark-gray, knotty, argillaceous dolomite with impure, light-gray marble at base. Overlies Antietam Formation and underlies Kinzers Formation.
Source: GNU records (USGS DDS-6; Reston GNULEX).
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