sideling hill road cut

Having spent considerable time in the western US it doesn’t seem that impressive to me but since I’ve been deprived of seeing geological strata for the past year I took a little detour on our family trip to North Carolina to check this road cut out. The Sideling Hill road cut is a 340-foot deep road cut where Interstate 68 cuts through Sideling Hill, about 6 miles west of Hancock in Washington County, Maryland. The Sideling Hill road cut is a 340-foot deep road cut where Interstate 68 cuts through Sideling Hill, about 6 miles west of Hancock in Washington County, Maryland. Immediate divestment from police and police departments. Photo credit. These rocks are a textbook example of the … Such folding resulted from the enormous compressional stresses developed in the Earth's crust by the collision of the North American and African continents. The Sideling Hill road cut exposes a section through the axis of a tightly folded syncline. More than 800 feet of strata in a tightly folded syncline are exposed in this road cut. It is notable as an impressive man-made mountain pass, visible from miles away and one of the best rock exposures in Maryland and indeed in the entire northeastern United States. Marker is on the westbound Sideling Hill Visitors Center (Interstate 68 at milepost 75) west of Exit 77 (Maryland Route 144), on the right when traveling west. Sideling Hill Welcome Center is along the westbound lane of I-68, adjacent to a large cut through a mountain. Sideling Hill is a tucked away spot at the Maryland-West Virginia border, south of interstate 68 between the Green Ridge State Forest and the Chesapeake and Ohio Canal National Historic Park. A syncline is a fold in which the strata on either side dip inward toward the axis. A syncline is a fold in which the strata on either side dip inward toward the axis. Such folding resulted from the enormous compressional stresses developed in the Earth's crust by the collision of the North American and African continents. April 30th, 2013 by WCBC Radio.

Geologists were ecstatic when the Sideling Hill Cut was completed. Sideling Hill Visitor Center (not currently open) is on Sideling Hill WMA. The center sits on the east side of Sideling Hill west of Hancock, where a 340-foot-deep cut was blasted out of the mountain rock to make way for Interstate 68. This Rest Area has everything others have in terms of rest area.

Sideling Hill is a syncline mountain, in a region of downward-folded (synclinal) rock strata between two upfolded anticlines. The cut was made in 1983.

It is notable as an impressive man-made mountain pass, visible from miles away, and is considered to be one of the best rock exposures in Maryland and the entire northeastern United States. The Sideling Hill rest area is located where the National Highway (I-68) cut through the mountain. They called it one of the best rock exposures in the entire country, comparable to the famous premier road cut …