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Native copper in Catoctin Formation metabasalt from the Virgin Mine in Pine Mountain, PA.
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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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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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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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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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