File:Grand Canyon of Yellowstonen edit1.jpg

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English: Grand Canyon at Yellowstone National Park. The colors in the canyon are also a result of hydrothermal alteration. The rhyolite in the canyon contains a variety of different iron compounds. When the old geyser basin was active, the "cooking" of the rock caused chemical alterations in these 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.
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Author Brocken Inaglory edited by Muhammad
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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current21:23, 16 April 2009Thumbnail for version as of 21:23, 16 April 20092,400 × 1,793 (2.86 MB)Muhammad Mahdi Karim (talk | contribs)== Summary == {{Information |Description=Grand Canyon at {{w|Yellowstone National Park}}.The colors in the canyon are also a result of hydrothermal alteration. The rhyolite in the canyon contains a variety of different iron compounds. When the old geyser

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