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Fixed-focal-distance image of the view out the front of my house.
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First in a series recording the onset of fall foliage in Virginia's Fort Valley.
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Just keeping tabs on the changes to my land over the years.
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This view shows the bedding plane of a slab of Massanutten Sandstone dipping into Passage Creek just upstream of Red Hole. For GigaPans of the larger site, please see: gigapan.com/gigapans/113761 and gigapan.com/gigapans/113759 Trace fossils can be observed in some places on this slab. Blue Hole ...
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Blue Hole is a popular swimming hole on Passage Creek in the northern part of George Washington National Forest, about 1 mile north (downstream) of Elizabeth Furnace, and 3 miles south of Waterlick, Virginia. The rock here is Silurian-aged Massanutten Sandstone. This site is just north (downstream) of Red Hole: ...
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Red Hole is a popular swimming hole on Passage Creek in the northern part of George Washington National Forest. The site is about one mile north (downstream) of Elizabeth Furnace, and three miles south of the "town" of Waterlick. The rock here is Silurian-aged Massanutten Sandstone. For another view, take a look ...
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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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The Paw Paw Tunnel on the C&O Canal exposes some fine geology, like these Brallier Formation slabs which, here, dip into the Tunnel Hollow, with a potential for breaking off and slipping down into the valley.
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The Paw Paw Tunnel on the C&O Canal exposes some fine geology, like these slickensides on a slab of the Brallier Formation: these formed due to flexural slip between layers as they folded during mountain building accompanying the Alleghanian Orogeny.
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The Paw Paw Tunnel on the C&O Canal exposes some fine geology.
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