A thick lenticular zone of hard red pebbly arkosic sandstone and conglomerate near the base of the Gettysburg Shale is named the Conewago Conglomerate Member. It extends from southwest of Airy Hill School in western York Co., PA, northeastward through Harmony Grove and Conewago Mountain to northwest of Strinestown. Maximum thickness is 7,300 ft. Age is Late Triassic.
Source: GNU records (USGS DDS-6; Reston GNULEX).
That part of the Gettysburg Formation designated Conewago Conglomerate Member by Stose and Jonas (1939) was examined at seven exposures and was not separable from typical Gettysburg lithologies. The name Conewago is not recognized and rocks in the area designated Conewago are part of the undifferentiated lower unnamed member of the Gettysburg Formation.
Source: GNU records (USGS DDS-6; Reston GNULEX).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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