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Form a panorama of Big Horn Hot Spring, Thermopolis; looking east across Big Horn River and the terraces of travertine to the "Red Beds' which are inclined southward on the flank of a sharp anticline whose apex lies to the left. From this anticline 18,600,000 gallons of sulphur water issues every 24 hours, having a temperature of 135 degrees F, and carrying calcium carbonate and other mineral matter in solution. In the distance in order from left to right, are the older Chugwater red beds, the Alcova marine limestone, gypsum and shale of the upper part of the Chugwater, the marine Sundance formation, (the basal sandstone is absent here), the Morrison formation and the sandstone correlated with the lower sandstone...
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Beds of the upper part of the Fort Union formation and lower part of the Wasatch formation exposed in the ravine that cuts through Blue Ridge in sec. 5, T. 46 N., R. 97 W. The conspicuous bed near the middle of the section is the massive conglomerate that forms the base of the Wasatch in this region. Hot Springs County, Wyoming. September 29, 1913. Plate 16 in U.S. Geological Survey. Professional paper 145. 1926.
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Frontier formation in Lysite Mountain anticline. Hot Springs County, Wyoming. 1914. Plate 5-B in U.S. Geological Survey. Bulletin 656. 1917.
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Form a panorama of Big Horn Hot Spring, Thermopolis; looking east across Big Horn River and the terraces of travertine to the "Red Beds' which are inclined southward on the flank of a sharp anticline whose apex lies to the left. From this anticline 18,600,000 gallons of sulphur water issues every 24 hours, having a temperature of 135 degrees F, and carrying calcium carbonate and other mineral matter in solution. In the distance in order from left to right, are the older Chugwater red beds, the Alcova marine limestone, gypsum and shale of the upper part of the Chugwater, the marine Sundance formation, (the basal sandstone is absent here), the Morrison formation and the sandstone correlated with the lower sandstone...
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Form a panorama of Big Horn Hot Spring, Thermopolis; looking east across Big Horn River and the terraces of travertine to the "Red Beds' which are inclined southward on the flank of a sharp anticline whose apex lies to the left. From this anticline 18,600,000 gallons of sulphur water issues every 24 hours, having a temperature of 135 degrees F, and carrying calcium carbonate and other mineral matter in solution. In the distance in order from left to right, are the older Chugwater red beds, the Alcova marine limestone, gypsum and shale of the upper part of the Chugwater, the marine Sundance formation, (the basal sandstone is absent here), the Morrison formation and the sandstone correlated with the lower sandstone...
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Limestone on south slope of Owl Creek Mountains on auto road between Thermopolis and Bannerville, Wyoming. Wyoming. 1921.
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View of canyon of Big Horn River south of Thermopolis, seen from train. Central Wyoming. June 1922.
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Panorama with image 2136. Terrace of mineral matter deposited by the hot sulphur water at Thermopolis. Wyoming. 1921.
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Basal sandstone and coal-bearing portion of the Mesaverde formation at north end of Grass Creek basin: sec. 5, T. 46 N., R. 98 W. Hot Springs County, Wyoming. September 11, 1912. Plate 7-D in U.S. Geological Survey. Professional paper 145. 1926.
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Upper part of the Meeteetse formation and lower part of the Lance formation along escarpment of north side of Prospect Creek: T.45 N., R. 99W. Hot Springs County, Wyoming. September 11, 1913. Plate 10-C in U.S. Geological Survey. Professional paper 145. 1926.
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Form a panorama of Big Horn Hot Spring, Thermopolis; looking east across Big Horn River and the terraces of travertine to the "Red Beds' which are inclined southward on the flank of a sharp anticline whose apex lies to the left. From this anticline 18,600,000 gallons of sulphur water issues every 24 hours, having a temperature of 135 degrees F, and carrying calcium carbonate and other mineral matter in solution. In the distance in order from left to right, are the older Chugwater red beds, the Alcova marine limestone, gypsum and shale of the upper part of the Chugwater, the marine Sundance formation, (the basal sandstone is absent here), the Morrison formation and the sandstone correlated with the lower sandstone...
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Massive sandstone of the Lance formation unconformably overlain by gravel of the Wasatch formation at the head of Iron Creek: sec. 8, T. 47 N., R. 100 W. Hot Springs County, Wyoming. 1912. Plate 10-D in U.S. Geological Survey. Professional paper 145. 1926.
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Hot sulphur water near Thermopolis, Wyoming. Used for irrigation. Wyoming. 1921.
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View of canyon of Big Horn River south of Thermopolis, seen from train. Central Wyoming. 1922.
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Blue-green algae in the hot sulphur water of Big Horn Hot Spring at Thermopolis. Big Horn Basin, Wyoming. 1922.
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Hot sulphur water near Thermopolis, Wyoming. Used for irrigation. Wyoming. 1921.
map background search result map search result map Massive sandstone of the Lance formation unconformably overlain by gravel of the Wasatch formation at the head of Iron Creek. Hot Springs County, Wyoming. 1912. Basal sandstone and coal-bearing portion of the Mesaverde formation at north end of Grass Creek basin. Hot Springs County, Wyoming. 1912. Upper part of the Meeteetse formation and lower part of the Lance formation along escarpment of north side of Prospect Creek. Hot Springs County, Wyoming. 1913. Beds of the upper part of the Fort Union formation and lower part of the Wasatch formation exposed in the ravine. Hot Springs County, Wyoming. 1913. Form a panorama of Big Horn Hot Spring, Thermopolis. Hot Springs County, Wyoming. 1922 Form a panorama of Big Horn Hot Spring, Thermopolis. Hot Springs County, Wyoming. 1922. Form a panorama of Big Horn Hot Spring, Thermopolis. Hot Springs County, Wyoming. 1922. Form a panorama of Big Horn Hot Spring, Thermopolis. Hot Springs County, Wyoming. 1922. Massive sandstone of the Lance formation unconformably overlain by gravel of the Wasatch formation at the head of Iron Creek. Hot Springs County, Wyoming. 1912. Basal sandstone and coal-bearing portion of the Mesaverde formation at north end of Grass Creek basin. Hot Springs County, Wyoming. 1912. Upper part of the Meeteetse formation and lower part of the Lance formation along escarpment of north side of Prospect Creek. Hot Springs County, Wyoming. 1913. Beds of the upper part of the Fort Union formation and lower part of the Wasatch formation exposed in the ravine. Hot Springs County, Wyoming. 1913. Form a panorama of Big Horn Hot Spring, Thermopolis. Hot Springs County, Wyoming. 1922 Form a panorama of Big Horn Hot Spring, Thermopolis. Hot Springs County, Wyoming. 1922. Form a panorama of Big Horn Hot Spring, Thermopolis. Hot Springs County, Wyoming. 1922. Form a panorama of Big Horn Hot Spring, Thermopolis. Hot Springs County, Wyoming. 1922.