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The Cumberland Narrows (or simply The Narrows [1]) is a water gap in western Maryland in the United States, just west of Cumberland. Wills Creek cuts through the central ridge of the Wills Mountain Anticline at a low elevation here between Wills Mountain to the north and Haystack Mountain to the south.
Wills Creek and Town Creek Watersheds in Pennsylvania and Maryland. Wills Creek drops off the Allegheny Mountains of southeastern Somerset County, Pennsylvania, beginning on the western slope of Savage Mountain [2] in Larimer Township. It flows into Northampton Township, passing through Mance, Philson Station, and Glencoe.
Wills Creek is a tributary of the Muskingum River, 92.2 mi (148.4 km) long, in eastern Ohio in the United States. Via the Muskingum and Ohio Rivers, it is part of the watershed of the Mississippi River. It drains an area of 853 mi 2 (2,209 km 2). [1] The United States Board on Geographic Names settled on
Wills Creek may refer to: Wills Creek (North Branch Potomac River), in Pennsylvania and Maryland; Wills Creek (Ohio), a tributary of the Muskingum River;
From 1899 until 1930, Wills Mountain was the site of the Wills Mountain Inn, a mansion featuring 46 bedrooms with private baths and a grand ballroom that was initially used as a fraternal clubhouse and informal country club. [2] In 1902, the property was sold to Dr. Henry Fry for conversion to a sanatorium. [3] The property burned down in 1930. [2]
Cumberland Quarry - Located in the Wills Creek Formation on the south side of Wills Creek, opposite Valley Street in Cumberland. There are two 20-foot-long crawlways located in a tightly folded section of the Wills Creek Formation, on the east face of the quarry. [3] Devils Den - Located south of Flintstone on the farm once owned by Harry ...
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The Wills Creek is defined as a moderately well bedded greenish-gray shale containing local limestone and sandstone zones, or more specifically as an olive to yellowish-gray, thin-bedded sandstone, calcareous shale, dolomite, argillaceous limestone, and sandstone. Red shale and siltstone occur in the lower part of the formation.