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Where Interstate 64 crosses the Blue Ridge, some fine exposures of Catoctin Formation greenstone may be found. For another perspective on the same location, check out this GigaPan: gigapan.com/gigapans/126934
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- 282
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- 32
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Where Interstate 64 crosses the Blue Ridge, there are terrific outcrops of Catoctin Formation greenstone. For another perspective on the same location, check out this GigaPan: gigapan.com/gigapans/126939
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- 268
- Explore Score
- 30
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Native copper in Catoctin Formation metabasalt from the Virgin Mine in Pine Mountain, PA.
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- 332
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- 21
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This is an exposure of the Catoctin formation at Point of Rocks in Maryland, on the north bank of the Potomac River. Point of Rocks is a prominent water gap cut by the Potomac River. The Catoctin formation is Neoproterozoic in age and was erupted as a series of flood basalts during the breakup of the Mesoproterozoic su...
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- 522
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- 1
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This is an exposure of the Catoctin formation at Point of Rocks in Maryland, on the north bank of the Potomac River. Point of Rocks is a prominent water gap cut by the Potomac River. The Catoctin formation is Neoproterozoic in age and was erupted as a series of flood basalts during the breakup of the Mesoproterozoic su...
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- 532
- Explore Score
- 37
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Devil's Racecourse in Ft. Ritchie, MD is a 700-meter-long blockfield created when the area experienced a periglacial climate during the Pleistocene. It is thought that boulders of Weverton quartzite from South Mountain on the west and Catoctin metabasalt from the east weathered out of their respective mountains an...
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- 299
- Explore Score
- 33
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Devil's Racecourse in Ft. Ritchie, MD is a 700-meter-long blockfield created when the area experienced a periglacial climate during the Pleistocene. It is thought that boulders of Weverton quartzite from South Mountain on the west and Catoctin metabasalt from the east weathered out of their respective mountains and wer...
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- 314
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- 1
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Devil's Racecourse in Ft. Ritchie, MD is a 700-meter-long blockfield created when the area experienced a periglacial climate during the Pleistocene. It is thought that boulders of Weverton quartzite from South Mountain on the west and Catoctin metabasalt from the east weathered out of their respective mountains and wer...
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- 339
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- 1
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This GigaPan was taken on Compton Peak in Shenandoah National Park, Virginia. The view of the camera is looking roughly west back up the hill towards the peak. These columns are in Catoctin metabasalt and are arguably the best examples of columnar jointing in Virginia. Image made as part of the MAGIC project (Mid-A...
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- 513
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- 1
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