Pennsylvania
Mt. Davis (Negro Mountain) |
Sedimentary |
Bedrock: Pottsville Sandstone |
Early Pennsylvanian |
White to gray sandstone and conglomerate. The Pottsville is folded by broad open folds in the Allegheny Mountains. At Mt. Davis the rocks dip eastward under younger rocks in the Berlin syncline. On the east side of the syncline, the formation reappears dipping west on Allegheny Mountain. Farther east, on the other side of the next anticline, the Pottsville dips east again to form the ridge of Big Savage Mountain and Backbone Mountain, Maryland (see Maryland highpoint). Surficial Geology: Unglaciated. However, tundra conditions during the Pleistocene produced stone rings caused by frost heaving. A good description of the process can be found at the Forbes State Forest website (see below). Soil Series: Hazleton very bouldery sandy loam : dark grayish-brown, well drained, channery sandy loam over yellow-brown subsoil. Formed from weathering of underlying bedrock, with rocks covering more than 60% of the area. This is the "state soil" of Pennsylvania. See photos at: http://soils.usda.gov/gallery/state_soils/#list |
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