File:BridalveilCreek.jpg
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Summary
| Description |
English: Yosemite National Park, California. Hanging valley of Bridalveil Creek, showing its pronounced form which is controlled, in large measure, by sparse diagonal joint structures. The valley has been occupied by ice, probably in the form of a more or less stagnant lobe of the main Yosemite Glacier, and is not believed to have been significantly altered by glacial erosion. |
| Date | circa 1913 |
| Source | http://libraryphoto.cr.usgs.gov/htmllib/btch196/btch196j/btch196z/btch196/mfe00168.jpg |
| Author | Matthes, F.E. |
37°42′N 119°38′W / 37.7°N 119.633°W
Licensing
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This image is in the public domain in the United States because it only contains materials that originally came from the United States Geological Survey, an agency of the United States Department of the Interior. For more information, see the official USGS copyright policy.
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File history
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 22:00, 27 July 2008 | | 1,033 × 1,400 (884 KB) | Eeekster | {{Information |Description={{en|1=Yosemite National Park, California. Hanging valley of Bridalveil Creek, showing its pronounced form which is controlled, in large measure, by sparse diagonal joint structures. The valley has been occupied by ice, probably |
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