Biotite-quartz-plagioclase gneiss interlayered with hornblende-quartz-plagioclase gneiss that outcrops along Bel Air Road north of Perry Hall in Baltimore Co., MD, here named Perry Hall Gneiss. Overlies Bradshaw Layered Amphibolite and Raspeburg Amphibolite of Baltimore Mafic Complex in northeast-southwest syncline. Age of unit given as Cambrian-Ordovician(?).
Source: GNU records (USGS DDS-6; Reston GNULEX).
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