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Pisgah Mountain, located along the southern fringe of northeastern Pennsylvania's Poconos region is also central to the Southern Anthracite Region of Pennsylvania— known as the site of the Richest Anthracite Seam, in the heart of the Southern Pennsylvania Anthracite Field and the geological province known as the Anthracite Upland section.
The Geology of Pennsylvania consists of six distinct physiographic provinces, three of which are subdivided into different sections. Each province has its own economic advantages and geologic hazards and plays an important role in shaping everyday life in the state.
The Bear Pond Mountains are a subrange in the Appalachian Mountains, that straddle Pennsylvania and Maryland in the United States. These mountains are a part of the Ridge and Valley Appalachians and reach their highest point at Cross Mountain (Pennsylvania) 2,062 feet (628 m). A unique geologic feature known as the "Punchbowl" occurs
The following is a list of the mapped bedrock units in Pennsylvania. The rocks are listed in stratigraphic order. The rocks are listed in stratigraphic order. [ 1 ]
Cross Mountain and Hearthstone Mountain 2,021 feet (616 m) which is on the Maryland side, form a unique geologic formation known as the "Punchbowl". This feature was created by the weathered shales of the Ordovician age in the center of a south-plunging anticline , having been eroded to expose a large amphitheater like feature (punchbowl).
Pages in category "Geologic formations of Pennsylvania" The following 44 pages are in this category, out of 44 total. ... This page was last edited on 30 November ...
Geological Society of America, Boulder, Colorado. Alan R. Geyer (1979) "Outstanding Geologic Features of Pennsylvania", Geological Survey of Pennsylvania; Charles H. Shultz (1999) The Geology of Pennsylvania, Geological Survey of Pennsylvania ISBN 0-8182-0227-0; Jere Martin (1997) Pennsylvania Almanac. Stackpole Books, ISBN 0-8117-2880-3
From the summit one can view the northernmost extension of the geologic province known as the Glaciated Low Plateaus section. The mountain itself is in the Ridge and Valley Appalachians. To access the summit one can take the Pinnacle Rock trail. The trailhead is on the west side of the mountain and is a nine hundred foot vertical gain.
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