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Gigapans

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  1. This is a replica Mayan relief carving

  2. 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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  3. 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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        Print Pricing
        $10.99 to $91.99
        Size
        1.11 Gigapixels
        Added
        April 21, 2013
        Date Taken
        April 21, 2013
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  4. The contact between the metasedimentary Fauquier Formation (uppermost marble member) and the overlying metavolcanic Catoctin Formation is exposed in an abandoned quarry north of Aldie, Virginia, across Goose Creek from Lime Kiln Road. The nature of this contact (is it conformable? does it show primary or tectonic struc...

  5. The contact between the metasedimentary Fauquier Formation (uppermost marble member) and the overlying metavolcanic Catoctin Formation is exposed in an abandoned quarry north of Aldie, Virginia, across Goose Creek from Lime Kiln Road. The nature of this contact (is it conformable? does it show primary or tectonic struc...

  6. The contact between the metasedimentary Fauquier Formation (uppermost marble member) and the overlying metavolcanic Catoctin Formation is exposed in an abandoned quarry north of Aldie, Virginia, across Goose Creek from Lime Kiln Road. The nature of this contact (is it conformable? does it show primary or tectonic struc...

  7. The contact between the metasedimentary Fauquier Formation (uppermost marble member) and the overlying metavolcanic Catoctin Formation is exposed in an abandoned quarry north of Aldie, Virginia, across Goose Creek from Lime Kiln Road. The nature of this contact (is it conformable? does it show primary or tectonic struc...

  8. A recumbent fold is exposed in the walls of an abandoned limestone quarry next to the Shenandoah River in Page County, Virginia.

  9. A recumbent fold is exposed in the walls of an abandoned limestone quarry next to the Shenandoah River in Page County, Virginia.

  10. Fanglomerate of the western Culpeper Basin.

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