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English: Grand Canyon and Yellowstone Fall at Yellowstone National Park. The canyon is up to 900 feet deep (275 m) and a half mile (0.8 km) in width. The canyon below the Lower Yellowstone Falls was at one time the site of a geyser basin that was the result of w:rhyolite w:lava flows, extensive faulting, and heat beneath the surface (related to the hot spot). The w:rhyolite in the canyon contains a variety of different iron compounds. Exposure to the elements caused the rocks to change colors. The rocks are, in effect, oxidizing; the canyon is rusting. The colors indicate the presence or absence of water in the individual iron compounds. Most of the yellows in the canyon are the result of iron present in the rock rather than sulfur.
Français : Le Grand Canyon de Yellowstone et la Lower Fall de la rivière Yellowstone, la plus grande chute d'eau du Parc national de Yellowstone avec une hauteur de 93 mètres. Le canyon atteint une profondeur maximale de 275 m pour une largeur de 800 m. Cette gorge correspond à un ancien bassin thermal, ce qui a résulté en l'oxydation de fer présent dans les rhyolites. Ce phénomène a abouti à une perte de cohésion de la roche, devenue facile à éroder, et en un changement de couleur, du rose vers le jaune.
Source Own work
Author Brocken Inaglory
Camera location44° 43′ 27.6″ N, 110° 30′ 17.6″ W Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo

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44°43'27.599"N, 110°30'17.600"W

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Date/TimeThumbnailDimensionsUserComment
current05:31, 26 January 2013Thumbnail for version as of 05:31, 26 January 20133,882 × 2,580 (9.29 MB)Slick-o-botBot: convert to a non-interlaced jpeg (see bug #17645)
00:11, 17 July 2008Thumbnail for version as of 00:11, 17 July 20083,882 × 2,580 (7.64 MB)Mbz1{{Information |Description={{en|1=e}} |Source=Own work by uploader |Author=Mbz1 |Date= |Permission= |other_versions= }} {{ImageUpload|full}}

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