| Abstract: | An outcrop of stratified slope deposits in Shenandoah National Park is described in detail. The Pleistocene age deposits are comprised of a mixture of clay to cobbles defining a series of offlapping wedges. Elongate clasts are oriented parallel to wedge boundaries except at the toe of the wedge, where they are oriented nearly vertical. The wedges represent sedimentation by freeze-thaw of ground ice. Thin layers of pebbly sand separate matrix-rich wedge deposits, which represent sheetfloods during periods of thaw. Thicker sand layers and lenses of clay are placed upslope of coarse-grained wedge fronts. This association represents ponding of water around the solifluction lobe topography during warm periods. Stratified slope deposits at an outcrop at a higher elevation lack the sandy sheetflood and pond deposits, whereas sheetflood fabrics dominate deposits at a lower elevation. These variations are attributed to differences in temperature at the different elevations. |
| Genre: | USGS Numbered Series |
| ProdID: | 56832 |
| Citation Author: | Smoot, Joseph P. |
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| Citation Edition: | Version 1.0, Online Only |
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| Citation Language: | ENGLISH |
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| Citation Online Only Flag: | Y |
| Citation Phsyical Description: | 49 p. |
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| Citation Series: | Open-File Report |
| Citation Series Code: | OFR |
| Citation Series Number: | 2004-1059 |
| Citation Search Results Text: | Sedimentary Fabrics of Stratified Slope Deposits at a Site near Hoover‘s Camp, Shenandoah National Park, Virginia; 2004; OFR; 2004-1059; Smoot, Joseph P. |
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| Citation Year: | 2004 |
| Type: | citation/reference |
| Text: | Sedimentary Fabrics of Stratified Slope Deposits at a Site near Hoover‘s Camp, Shenandoah National Park, Virginia; 2004; OFR; 2004-1059; Smoot, Joseph P. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/usgs_thumb.jpg |
| URL (INDEX PAGE): | http://pubs.usgs.gov/of/2004/1059/ |
| Date Other: | Thu, 1 Jul 2004 00:00 -0500 |
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