View of Cinnabar Mountain and the Devil's Slide on the Yellowstone. Park County, Montana. 1871.
Dates
Date Taken
1871
Summary
Album caption and index card: View of Cinnabar Mountain and the Devil's Slide on the Yellowstone, 10 miles above the second canyon. It is a mountain of alternate beds of limestone, sandstone, quartzites and volcanic dikes, elevated to a very nearly vertical position, with the softer strata so worn away as to leave the harder and more enduring ridges standing. View includes only the central portion of the long series of ridges. Prominent among them are two parallel walls, 50 feet apart and 200 feet in height, running up the mountain side 1,500 feet. Between the walls on one side is a band of bright vermilion-tinted clay, which has been mistaken for cinnabar, and hence the name Cinnabar Mountain. Park County, Montana. 1871. Descriptive [...]
Summary
Album caption and index card: View of Cinnabar Mountain and the Devil's Slide on the Yellowstone, 10 miles above the second canyon. It is a mountain of alternate beds of limestone, sandstone, quartzites and volcanic dikes, elevated to a very nearly vertical position, with the softer strata so worn away as to leave the harder and more enduring ridges standing. View includes only the central portion of the long series of ridges. Prominent among them are two parallel walls, 50 feet apart and 200 feet in height, running up the mountain side 1,500 feet. Between the walls on one side is a band of bright vermilion-tinted clay, which has been mistaken for cinnabar, and hence the name Cinnabar Mountain. Park County, Montana. 1871.
Descriptive Catalog of the Photographs of the United States Geological Survey of the Territories, W. H. Jackson, Photographer, Second Edition Illustrated, 1871 Series, page 24, Nos. 210- 13: Different views of Cinnabar Mountain and the Devil's Slide, ten miles above the second canyon. It is a mountain of alternate beds of limestone, sandstone, quartzites and volcanic dikes, elevated to a very nearly vertical position, with the softer strata so worn away as to leave the harder and more enduring ridges standing. Our views include only the central portion of the long series of ridges. Prominent among them are two parallel walls, fifty feet apart and two hundred in height, running up the mountain side 1,500 feet. Between the walls on one side is a band of bright vermilion-tinted clay, which has been mistaken for cinnabar, and hence the name Cinnabar Mountain.
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Related External Resources
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Descriptive catalogue of the photographs of the United States Geological Survey of the Territories for the years 1869 to 1875, inclusive: Miscellaneous publications - No. 5
Available in the U.S. Geological Survey Denver Library Photographic Collection, Jackson, W.H. Collection.
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