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  1. Massanutten Sandstone, folded into an anticline. To view a sample of the Massanutten Sandstone in macro detail, try this: gigapan.com/gigapans/126687

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  2. Massanutten Sandstone, folded into an anticline. To view a sample of the Massanutten Sandstone in macro detail, try this: gigapan.com/gigapans/126687

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

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

  6. Eocene limestones folded into an anticline. Paleocene and Upper Cretaceous rocks are in the core of the anticline. Alzina is in lower left.

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  7. Looking at an anticline in the Ordovician-aged Edinburg Formation from Frederick County, Virginia, on the western shore of Opequon Creek, gazing across into Clarke County. Strata are Ordovician; deformation is Alleghanian (late Paleozoic). Another set of folds is just upstream: gigapan.org/gigapans/120300 ...

  8. This outcrop of the Tuscarora Sandstone arched up along the Hanging Rock Anticline, occurs west of Wardensville, West Virginia, along Corridor H, the new section of Route 55. Perspective is looking along strike to the south/southwest.

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  9. This outcrop is found on South Page Valley Road, near the intersection with Bixlers Ferry Road, west of the South Fork of the Shenandoah River and east of Massanutten Mountain. It shows lower Martinsburg Formation limy shale (late Ordovician depositional age) folded and cleaved during Alleghanian mountain-building (lat...

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  10. Folded and faulted sequence of Carboniferous (Westphalian) sandstons and shales from the Bude Formation, exposed north of the seapool at Summerleaze Beach in Bude, Cornwall, England. The Bude Formation was deposited in a basin at the northern edge of the closing Rheic Ocean and was then deformed in the Variscan orogeny...

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