Maryland
Backbone Mountain |
Sedimentary |
Bedrock: Pottsville Sandstone |
Pennsylvanian |
Massive, light gray conglomerate and thin-bedded, gray to white sandstone with thin coal seams and minor shale horizons (cyclothems). The disconformable contact with the underlying red shales and sandstones of the Mauch Chunk Formation lies within 100 meters west of the summit ridge, which represents part of the Catskill delta, deposited as sediments eroded from mountains formed by the Acadian Orogeny along the eastern margin of Laurentia. The still older Devonian Jennings marine shale is exposed in the valley to the west at Mountain Lake Park, in the center of the eroded crest of an anticline. All these rocks were folded in the late Paleozoic Alleghenian Orogeny into the long canoe-shaped anticlines and synclines typical of the Ridge and Valley Province. Surficial Geology: South of the limit of Pleistocene glaciation Soil Series: Stony rough land: local pockets of soil between numerous outcrops, not differentiated on the soil survey map. |
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