File:Hot springs travertine (Holocene; Rattlesnake Mountain Uplift, west of Cody, Wyoming, USA) 5 (31274779336).jpg
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Summary[edit]
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| Description |
Hot springs travertine from the Holocene of Wyoming, USA. (21.8 cm across at its widest) Travertine is a crystalline-textured, chemical sedimentary rock composed of calcium carbonate (calcite). It forms principally in cave environments and is the most common variety of speleothem (stalactites, stalagmites, etc.). Travertine also forms at some springs, either hot springs or cold springs. This sample is from a weathered, extinct hot spring travertine mound on the western margin of Wyoming's Rattlesnake Mountain Uplift (a.k.a. Rattlesnake Mountain Anticline). The uplift is part of a extensive set of mountain ranges from New Mexico to western Canada that were formed during the Laramide Orogeny (late Mesozoic to mid-Cenozoic). Other inactive hot springs travertine mounds occur on the eastern side of the uplift. Nearby, some active hot springs occur on the western side of the town of Cody. The surface facing the viewer is covered with irregular ridges. This is an original flow surface - the ridges are small terraces (= small-scale rimstone dams). Hot spring water originally flowed "downward". Locality: float from roadcut on the northern side of Rt. 16 / 20, just west of third tunnel west of Cody, next to Buffalo Bill Reservoir, central Park County, northwestern Wyoming, USA (44° 30' 04.65" North latitude, 109° 11' 027.28" West longitude) |
| Date | |
| Source | Hot springs travertine (Holocene; Rattlesnake Mountain Uplift, west of Cody, Wyoming, USA) 5 |
| Author | James St. John |
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This image was originally posted to Flickr by James St. John at https://flickr.com/photos/47445767@N05/31274779336 (archive). It was reviewed on 6 December 2019 by FlickreviewR 2 and was confirmed to be licensed under the terms of the cc-by-2.0. |
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 03:19, 6 December 2019 | | 3,565 × 2,213 (6.09 MB) | Ser Amantio di Nicolao (talk | contribs) | Transferred from Flickr via #flickr2commons |
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