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  1. 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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  2. 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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      30

  3. 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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      208
      Explore Score
      34

  4. 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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      35

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        Print Pricing
        $11.99 to $115.99
        Size
        1.66 Gigapixels
        Added
        April 18, 2013
        Date Taken
        April 17, 2013
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  5. 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...

  6. 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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  7. 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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      239
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      29

  8. This exposure of the Lower Martinsburg shows bedding within the strongly cleaved limy slate.

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  9. This sample is of nice structural interest. It was a shaly limestone, but then it got squeezed. Foliation developed at an angle to bedding, meaning that technically the rock now bears slaty cleavage. It's still a limestone, compositionally, but the well-developed foliation means that it's texturally a slate. Sampling l...

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  10. Complex kink folds in the Lower Devonian fine-grained, siliciclastic metasediments of the core of the High-Ardenne Slate Belt (Belgium).

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        Size
        0.45 Gigapixels
        Added
        November 21, 2011
        Date Taken
        November 19, 2011
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