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Gigapans

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  1. Sherburne Formation and Genesee Group

  2. Acadian turbidites, folded during the Alleghanian Orogeny. Look for slickensides, trace fossils, turbidity current structures. For more information on the Brallier, check out this map of the location: ngmdb.usgs.gov/ngm-bin/pdp/zui_viewer.pl?id=8643 Will open in a new tab or window

  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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      142
      Explore Score
      33

  4. 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

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      0
      Comments
      Snapshots
      Total Views
      183
      Explore Score
      32

  5. 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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      Comments
      Snapshots
      Total Views
      158
      Explore Score
      36

  6. 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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      270
      Explore Score
      36

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

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      Total Views
      147
      Explore Score
      25

  8. 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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      167
      Explore Score
      37

  9. 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

  10. 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
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