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Brachiopod body fossils in the Ridgeley Member of the Old Port Formation, a Devonian sandstone (quartz arenite) which outcrops in Maryland, Pennsylvania, and West Virginia. This outcrop is in a railroad cut on the Great Allegheny Passage, approximately one mile northeast of the intersection of Cash Valley Road with ...
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This great little anticline is one of several accessable from the Veach Gap trail in George Washington National Forest, Fort Valley, Virginia. The rocks are from the Massanutten formation, a Silurian quartz arenite to quartzite. The folds seen here are parasitic folds which relate to the larger Massanutten Synclinorium...
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The Massanutten sandstone is a Silurian-aged passive margin deposit that is correlative to the Tuscarora Formation of the western Valley & Ridge province. A bed is exposed here in a subvertical orientation along the Woodstock Tower Road, near its summit. Perspective is looking across strike to the west-northwest. Trace...
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This outcrop of the Tuscarora Sandstone arched up along the Hanging Rock Anticline, occurs west of Wardensville, West Virginia, along Corridor H, the new section of Route 55. Perspective is looking along strike to the south/southwest.
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The Massanutten sandstone is a Silurian-aged passive margin deposit that is correlative to the Tuscarora Formation of the western Valley & Ridge province. A bed is exposed here in a subvertical orientation along the Woodstock Tower Road, near its summit. Perspective is looking across strike to the west-northwest. Trace...
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The Massanutten sandstone is a Silurian-aged passive margin deposit that is correlative to the Tuscarora Formation of the western Valley & Ridge province. A bed is exposed here in a subvertical orientation along the Woodstock Tower Road, near its summit. Perspective is looking across strike to the west-northwest. Trace...
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This exposure of tilted strata within the Massanutten Sandstone is found on the north side of Passage Creek above Red Hole, within the Passage Creek Day Use Area of the George Washington National Forest, Virginia. To view a sample of the Massanutten Sandstone in macro detail, try this: gigapan.com/gigapans/1...
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This exposure of tilted strata within the Massanutten Sandstone is found on the north side of the Fort Valley Road near Red Hole, within the Passage Creek Day Use Area of the George Washington National Forest, Virginia. To view a sample of the Massanutten Sandstone in macro detail, try this: gigapan.com/giga...
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Red Hole is a popular swimming hole on Passage Creek in the northern George Washington National Forest, about a mile north of Elizabeth Furnace, and 3 miles south of Waterlick. The rock here is Silurian-aged Massanutten Sandstone. For another view, take a look at this GigaPan: gigapan.com/gigapans/113761...
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This great little anticline is one of several accessable from the Veach Gap trail in George Washington National Forest, Fort Valley, Virginia. The rocks are from the Massanutten formation, a Silurian quartz arenite to quartzite. The folds seen here are parasitic folds which relate to the larger Massanutten Synclinorium...
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- 0
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- 259
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- 1