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University of Michigan Library
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The geology of Bedford and Fulton counties.
by:John J. Stevenson
General Books publication date: 2009 Original publication date: 1882 Original Publisher: Pub. by the Board of Commissioners for the Second Geological Survey Subjects: Geology Science / Earth Sciences / General Science / Earth Sciences / Geology Notes: This is a black and white OCR reprint of the original. It has no illustrations and there may be...
General Books publication date: 2009 Original publication date: 1882 Original Publisher: Pub. by the Board of Commissioners for the Second Geological Survey Subjects: Geology Science / Earth Sciences / General Science / Earth Sciences / Geology Notes: This is a black and white OCR reprint of the original. It has no illustrations and there may be typos or missing text. When you buy the General Books edition of this book you get free trial access to Million-Books.com where you can select from more than a million books for free. Excerpt: The Cove fault. This interesting phenomenon deserves some special refer ence here, though all the details obtained are given in the chapters on Ayr, Todd and Dublin townships of Pulton county. This fault originates in Dickey's mountain at probably one mile south from Big Spring run, and continues thence for about 11 or 12 miles in a rudely northern direction to within somewhat more than a mile of the Huntingdon county line, where it is lost amid the Devonian shales. It crosses the general strike of the rocks, so that in going northward from Dickey's mountain it cuts off the high groups in succession and after reaching the undisturbed portion of Little Scrub ridge it cuts off the same groups a second time. This condition is due to the semi-oval form of outcrops on the west side of the Cove anticlinal. From the origin of the fault to where it passes into the Clinton on the northwest side of Little Scrub ridge it holds in its jaws the upper beds of the white Medina. This rock forms a projecting wall from 50 to 200 feet wide. It forms Lowrie'' s knob, the northern point of Dickey's mountain; thence for half a mile it is missing; but, soon re-appearing, it is readily traceable to the Bedford pike as a low irregular ridge. At the pike it becomes a high ridge, and thence, as part of Little Scrub ridge, it can be followed by its jagged crest to where the fault passes beyond the Medina of that ridge. To trace the fault to its origin...
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