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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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      142
      Explore Score
      33

  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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    • Stats

      Favorites
      0
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      Snapshots
      Total Views
      183
      Explore Score
      32

  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.

    • Stats

      Favorites
      0
      Comments
      Snapshots
      Total Views
      158
      Explore Score
      36

  4. Cross-sectional view of folded Martinsburg Formation beds (XXX°, XX° right hand rule).

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      1
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      Total Views
      148
      Explore Score
      25

  5. Cross-sectional view of folded Martinsburg Formation beds . On the left (south), the bedding is oriented 030°, 38° (right hand rule). On the right (north), it's oriented 245°, 30° (right hand rule).

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      1
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      167
      Explore Score
      37

  6. Cross-sectional view of inclined Martinsburg Formation beds (020°, 62° right hand rule). Take a look and ask yourself: What's the structure doing here? :)

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      1
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      Total Views
      102
      Explore Score
      28

  7. Cross-sectional view of subvertical Martinsburg Formation beds (220°, 80° right hand rule).

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      1
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      Total Views
      98
      Explore Score
      25

  8. This is a subvertical bedding plane (220° / 80°, right hand rule) of the late Ordovician Martinsburg Formation, showing the bottom of a turbidite bed. Several features are visible in this bottom-up perspective.

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      Total Views
      209
      Explore Score
      34

  9. This is a subvertical bedding plane (220° / 80°, right hand rule) of the late Ordovician Martinsburg Formation, showing the bottom of a turbidite bed. Several features are visible in this bottom-up perspective.

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      Favorites
      1
      Comments
      Snapshots
      Total Views
      206
      Explore Score
      32

  10. 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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      0
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      Total Views
      304
      Explore Score
      31
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