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About: Bear Pond Mountains     Goto   Sponge   NotDistinct   Permalink

An Entity of Type : umbel-rc:MountainRange, within Data Space : dbpedia.demo.openlinksw.com associated with source document(s)

Type: Thingplacedbo:Locationschema:Mountainschema:Placenatural placeMountainyago:WikicatMountainRangesOfMarylandyago:WikicatMountainRangesOfPennsylvaniageo:SpatialThingyago:GeologicalFormation109287968yago:Object100002684yago:PhysicalEntity100001930yago:Range109403734yago:YagoGeoEntityyago:YagoPermanentlyLocatedEntitymountainumbel-rc:MountainRange New Facet based on Instances of this Class

The Bear Pond Mountains are a sub-range 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 in this range. 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). Cross and Hearthstone Mountain are made of hard resistant quartzite of the Tuscarora Formation of the Silurian age, which form the walls of the bowl.