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Gigapans

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  1. 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 Will open in a new tab or window The same contact can be seen in the vicinity of Strasburg, Virginia, here: www.gigapan.com/gi...

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      166
      Explore Score
      42

  2. An exposure of highly foliated metasedimentary rock (metagraywacke) of the Laurel Formation in Broad Branch, part of Rock Creek Park, in northwest Washington, DC.

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      205
      Explore Score
      38

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        Print Pricing
        $10.99 to $91.99
        Size
        1.97 Gigapixels
        Added
        April 25, 2013
        Date Taken
        April 24, 2013
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  3. An exposure of highly foliated metasedimentary rock (metagraywacke) of the Laurel Formation in Broad Branch, part of Rock Creek Park, in northwest Washington, DC.

    • Order Print

    • Stats

      Favorites
      0
      Comments
      Snapshots
      Total Views
      165
      Explore Score
      40

      • Meta

        Print Pricing
        $10.99 to $91.99
        Size
        1.21 Gigapixels
        Added
        April 25, 2013
        Date Taken
        April 24, 2013
        Categories
         
        Tags

  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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      Total Views
      139
      Explore Score
      33

  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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      0
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      Snapshots
      Total Views
      174
      Explore Score
      32

  6. 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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      0
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      Total Views
      154
      Explore Score
      36

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

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      145
      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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      165
      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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      Total Views
      100
      Explore Score
      28

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

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      96
      Explore Score
      25
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