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  1. Large road cut exposing folded bedding of the Ordovician Bascom Formation. Road cut exposed on the south side of Rt 279 (Bennington Bypass). Bascom Formation - Interbedded dolomite, limestone or marble, calcareous sandstone, quartzite and limestone breccia; irregular dolomitic layers, thin sandy laminae, and slaty or...

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      75
      Explore Score
      52

  2. Quartz arenite of the Tuscarora Formation (Silurian-age) exposed in a road cut through the Hanging Rock Anticline, West Virginia.

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      Total Views
      154
      Explore Score
      27

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        Print Pricing
        $6.99 to $67.99
        Size
        0.79 Gigapixels
        Added
        April 21, 2013
        Date Taken
        April 21, 2013
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  3. West Virginia, Corridor H. Can you find fault in this GigaPan? See also: gigapan.com/gigapans/111249 gigapan.com/gigapans/98672

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      Total Views
      135
      Explore Score
      24

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        Print Pricing
        $10.99 to $91.99
        Size
        0.98 Gigapixels
        Added
        April 21, 2013
        Date Taken
        April 21, 2013
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  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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      Total Views
      342
      Explore Score
      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. Cross-sectional view of folded Martinsburg Formation beds (XXX°, XX° right hand rule).

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      1
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      Total Views
      175
      Explore Score
      24

  6. 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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      Total Views
      197
      Explore Score
      37

  7. 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
      123
      Explore Score
      27

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

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      1
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      Total Views
      124
      Explore Score
      23

  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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      Total Views
      258
      Explore Score
      32

  10. 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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    • Stats

      Favorites
      1
      Comments
      Snapshots
      Total Views
      239
      Explore Score
      32
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