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I have made many GigaPans--of landscapes, trees, fencerows, underbrush--in Bluemont, Virginia, about 45 miles "as the crow flies" west of Washington, D.C. Bluemont used to be just a little village and a lot of farmland. Now speculative subdivision development encroaches on that farmland. On the left, in ...
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May 14, 2013. View 2 of 3 For a version of this same view, but with flood waters raging, see this GigaPan: gigapan.com/gigapans/129543
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- 63
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- Folded contact between New Market Formation (lower) and Lincolnshire Formation (upper), Staunton, Virginia by Callan Bentley
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A lovely exposure (though rather harshly lit) of the contact between two Cambro-Ordovician limestones in the Shenandoah Valley. Geologic map of the site is here: ngmdb.usgs.gov/ngm-bin/pdp/zui_viewer.pl?id=14868
The same contact can be seen in the vicinity of Strasburg, Virginia, here:
www.gigapan.com/gi...-
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- Contact between Fauquier Formation marble and Catoctin Formation greenstone, near Lime Kiln Road, Virginia by Callan Bentley
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The contact between the metasedimentary Fauquier Formation (uppermost marble member) and the overlying metavolcanic Catoctin Formation is exposed in an abandoned quarry north of Aldie, Virginia, across Goose Creek from Lime Kiln Road. The nature of this contact (is it conformable? does it show primary or tectonic struc...
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- 448
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- 38
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This is a highly deformed section of the Devonian Foreknobs Formation exposed near Bergton Va. The Foreknobs Formation ( formerly known as the Chemung) is a mixed package of brownish red to grey sandstone siltstone shale and minor conglomerate. This formation is part of the Catskill Delta, a shallowing upward sequence...
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- 587
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- 38
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After a day and night of heavy rainfall Jan. 30, Passage Creek flooded its banks in the Fort Valley on the morning of January 31, 2013. For another view (lower on the hill), try this GigaPan: gigapan.com/gigapans/122529
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- 1000
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Outcrop of the late-Ordovician-aged Martinsburg Formation (turbidites/flysch) shed off the Taconian Orogen to the east into the adjacent deep marine basin. The strata were later tilted and cleaved during Alleghanian mountain-building.
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- 155
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A recumbent fold is exposed in the walls of an abandoned limestone quarry next to the Shenandoah River in Page County, Virginia.
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- 239
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- 35
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Close up of some of the breccia cemented by siliceous and iron/manganese oxide cements. Image brought to you by the Mid-Atlantic Geo-Image Collection (M.A.G.I.C.).
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A recumbent fold is exposed in the walls of an abandoned limestone quarry next to the Shenandoah River in Page County, Virginia.
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- 463
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