Named the Spring Mount sandstone member of the Bald Eagle sandstone in central PA. Unit is upper member of formation in vicinity of Tyrone Gap and is a ridge forming unit. Overlies Centennial School sandstone and shale member of the Bald Eagle, interfingers with the Lost Run conglomerate to the east, and underlies the Juniata strata. The Spring Mount is of Late Ordovician age.
Source: GNU records (USGS DDS-6; Reston GNULEX).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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