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Group: Mid-Atlantic Geo-Image Collection (M.A.G.I.C.)

Fossils

2d8a6bc32a428c0ed9cdb2ec18791750

65 GigaPansViews

Traces of long-dead flora and fauna.

Created by
Robin Rohrback-Schiavone
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0.473806 gigapixels
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195
Dated added
November 18, 2012
Categories
geology, macro, nature
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  1. Characteristic fossils of the Buda Formation may be seen in loose blocks at an abandoned quarry on the north side of the Cristo Rey laccolith.

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  2. Characteristic fossils of the Buda Formation may be seen in loose blocks at an abandoned quarry on the north side of the Cristo Rey laccolith.

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  3. Characteristic fossils of the Buda Formation may be seen in loose blocks at an abandoned quarry on the north side of the Cristo Rey laccolith.

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        0.46 Gigapixels
        Added
        May 07, 2013
        Date Taken
        May 04, 2013
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  4. 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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  5. Syncline adjacent to the Patterson Creek Mountain Anticline, exposed in West Virginia, along Corridor H. For other views of this site, see: gigapan.com/gigapans/103106 gigapan.com/gigapans/103090 gigapan.com/gigapans/103089 gigapan.com/gigapans/91448

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        Added
        April 21, 2013
        Date Taken
        April 21, 2013
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  6. Shot at fixed focal distance, which means that most of this image is out-of-focus. Still - nice fossils.

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  7. Cruziana trace fossils, donated by Alan Pitts.

  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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  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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  10. This is a "doomed" outcrop of the Miocene-aged (~14 Ma) Calvert Formation on the western shore of Chesapeake Bay. "Bed 14," a distinctive fossiliferous unit, is exposed here thanks to the effort of one of the local landowners. In a month or two, this entire outcrop will be permanently covered with "hard stabilization" ...

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