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All of Bedford County lies far to the south of the terminal moraine, and thus it was never glaciated (PA Geological Survey Map 59). However, during the Pleistocene epoch, or "Ice Age," periglacial (meaning "around glacier" or simply "cold") processes dominated. Most of the county was most likely a tundra at that time. The many boulder fields ...
English: This is a locator map showing Bedford County in Pennsylvania. For more information, ... Geology of Bedford County, Pennsylvania; Harrison Township, Bedford ...
Bedford County was created on March 9, 1771, from part of Cumberland County and named in honor of Fort Bedford. The 1767 Mason–Dixon line had stabilized the southern border with Maryland. In the aftermath of the American Revolution , the population increased largely due to emigration.
Chestnut Ridge is an elongate hill trending northeast-southwest in west-central Bedford County, Pennsylvania. It is partially forested with rural homes, farms, and notably apple orchards. Four small towns surround it: Schellsburg, New Paris, Fishertown, and Pleasantville.
The following is a list of the mapped bedrock units in Pennsylvania. The rocks are listed in stratigraphic order. ... Formation name Member name Map symbol [2 ...
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Colerain valley (shown as "Friends Cove" on topographic maps) is an anticlinal valley, with Evitts Mountain and Tussey Mountain forming the limbs. The Silurian Tuscarora Formation, a hard sandstone, outcrops at the crests of the ridges and is stratigraphically higher and thus younger than the rest of the bedrock in the valley.
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.