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Summary
| Description |
Shear or herring-bone crevasses on the Emmons Glacier; such crevasses often form near the edge of a glacier where interactions with underlying or marginal rock impede flow. In this case, the impediment appears to be some distance from the near margin of the glacier.
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| Date | 8 August 2002, 14:45 −07:00 |
| Source | Own work |
| Author | Walter Siegmund (talk) |
| Camera location |   | View this and other nearby images on: OpenStreetMap |  |
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Permission is granted to copy, distribute and/or modify this document under the terms of the GNU Free Documentation License, Version 1.2 or any later version published by the Free Software Foundation; with no Invariant Sections, no Front-Cover Texts, and no Back-Cover Texts. A copy of the license is included in the section entitled GNU Free Documentation License. |
  
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This file is licensed under the Creative Commons Attribution-Share Alike 3.0 Unported license. | |
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 23:15, 11 May 2013 | | 1,536 × 1,024 (584 KB) | Wsiegmund | Adobe Photoshop Elements 11.0; 30% Auto Smart Fix, Adjust Lighting/Shadows/Highlights, Levels, Reduce noise tools |
| 23:02, 11 May 2013 |  | 1,536 × 1,024 (653 KB) | Wsiegmund | {{Information |Description = {{en|Shear or herring-bone crevasses on the Emmons Glacier; such crevasses often form near the edge of a glacier where interactions with underlying or marginal rock impede flow. In this case, the impediment appears ... |
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