1. Skip to navigation
  2. Skip to content
  3. Skip to sidebar

Gigapans

NEW! Print your gigapan now!
Go to page:

  1. Roadcut in shales south of Wilson Lake, Kansas. Can you identify it's proper place in the stratigraphy (www.kgs.ku.edu/Publications/Bulletins/189/09_meso.html#CRET Will open in a new tab or window) of the region?

    • 8815-210x140

    • Stats

      Favorites
      2
      Comments
      3
      Snapshots
      8
      Total Views
      12905
      Explore Score
      112

  2. 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).

    • Stats

      Favorites
      1
      Comments
      Snapshots
      Total Views
      202
      Explore Score
      37

  3. 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

  4. Cambrian-aged Harpers Formation meta-mudstone exposed on the property of Arlington, Virginia's outdoor education facility, the Phoebe Hall Knipling Outdoor Lab.

    • Order Print

    • Stats

      Favorites
      0
      Comments
      Snapshots
      Total Views
      347
      Explore Score
      35

      • Meta

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

  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.

    • Stats

      Favorites
      0
      Comments
      Snapshots
      Total Views
      207
      Explore Score
      34

  6. Here is the base of the Foreknobs section exposed along rt 50 near Chambersville Virginia on the east limb of the Mt Pleasent Syncline. Here is shown the lowest massive marine sandstone which seperates itself from silty/sandy turbidites of the Brallier Formation. This Image is part of the Mid Atlantic Geo-Imagery Col...

  7. 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.

    • Order Print

    • Stats

      Favorites
      0
      Comments
      Snapshots
      Total Views
      259
      Explore Score
      32

  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.

    • Order Print

    • Stats

      Favorites
      1
      Comments
      Snapshots
      Total Views
      239
      Explore Score
      32

  9. 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.

    • Order Print

    • Stats

      Favorites
      0
      Comments
      Snapshots
      Total Views
      188
      Explore Score
      31

  10. 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.

    • Order Print

    • Stats

      Favorites
      0
      Comments
      Snapshots
      Total Views
      239
      Explore Score
      30
Go to page: