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The Glass Mountain is a geologic feature in Lower Cathedral Valley of Capitol Reef National Park consisting of large selenite (gypsum) crystals forming a mound or plug 15 feet high. Gypsum was deposited as sea water evaporated 165 million years ago and then buried under other sediments. The gypsum migrated upwards through fractures in the sediments forming layers and, very rarely, domes like the Glass Mountain. There is only one exposed selenite plug within the park and one other just outside which has been reduced to ground level by collectors.

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  • Glass Mountain (Utah) (en)
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  • The Glass Mountain is a geologic feature in Lower Cathedral Valley of Capitol Reef National Park consisting of large selenite (gypsum) crystals forming a mound or plug 15 feet high. Gypsum was deposited as sea water evaporated 165 million years ago and then buried under other sediments. The gypsum migrated upwards through fractures in the sediments forming layers and, very rarely, domes like the Glass Mountain. There is only one exposed selenite plug within the park and one other just outside which has been reduced to ground level by collectors. (en)
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  • http://commons.wikimedia.org/wiki/Special:FilePath/Glass_Mountain_(Capitol_Reef_National_Park).jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Glass_Mountain_and_Temple_of_the_Sun.jpg
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  • Capitol Reef Visitor Center, elevation , 1981-2010 normals, extremes 1981-2019 (en)
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  • 38.4547 -111.1919
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  • The Glass Mountain is a geologic feature in Lower Cathedral Valley of Capitol Reef National Park consisting of large selenite (gypsum) crystals forming a mound or plug 15 feet high. Gypsum was deposited as sea water evaporated 165 million years ago and then buried under other sediments. The gypsum migrated upwards through fractures in the sediments forming layers and, very rarely, domes like the Glass Mountain. There is only one exposed selenite plug within the park and one other just outside which has been reduced to ground level by collectors. (en)
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