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Cambrian-aged Harpers Formation meta-mudstone exposed on the property of Arlington, Virginia's outdoor education facility, the Phoebe Hall Knipling Outdoor Lab.
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- 254
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- 37
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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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- 152
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- 36
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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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- 139
- Explore Score
- 33
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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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- Total Views
- 173
- Explore Score
- 32
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Rhosydd is one of the larger slate mines near Blaenau Ffestiniog, North Wales. Of the original 14 levels, 5 are permanently flooded and around 100 chambers are still accessible. This incline is unusual in having wide gauge rails carrying slate trucks on a wagon while a heavy counterbalance wagon ran on narrower rails s...
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- 1
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- 184
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- 31
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This outcrop of the late Ordovician Martinsburg Formation is located on Route 644 in Shenandoah County, about 20 feet above the North Fork of the Shenandoah River. GigaPan Stitch seems to have had some issues putting it together, which is frustrating. Still, there's a lot to be seen. At this outcrop, bedding is o...
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- 298
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- 31
- Martinsburg Formation, Millner Road (near Deer Rapids Road), Shenandoah County, Virginia by Callan Bentley
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This outcrop of the late Ordovician Martinsburg Formation is located on Route 644 in Shenandoah County, about 60 feet above the North Fork of the Shenandoah River. At this outcrop, bedding is oriented 042°, 72° (right hand rule: it strikes N42°E, and dips 72° to the southeast). Cleavage is oriented 212°, 83° (...
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- 186
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- 29
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Axial planar cleavage-bedding plane relationships in the hinge of the West Castleton Syncline, Poultney Formation, Vermont slate belt
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- 3385
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- 1
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The West Castleton Fold was the subject of my second ever (non-robotic) GigaPan (share.gigapan.org/viewGigapan.php?id=1204).This shot illustrates the axial region of a recumbant syncline in the Poultney Formation of the Giddings Brook Slice of the Taconic Allochthon. This outcrop is a textbook example of axia...
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- 4
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- 3068
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- 1
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This is an abondoned quarry located to the east of West Pawlet, Vermont exposing an east dipping fold limb in the St Catherine Formation. The slight blue hue to the color is characteristic for most drowned quarries in the area and a result of the high clay content in the water.
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- 2026
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- 1
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