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Panorama with Images 379, 380, and 382. View south and east from north end of Skyline Rim (Ferron sandstone scarp). Wayne County, Utah. 1935.
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Panorama with Images 518 and 519. View north and northeast across Cedar Creek. Wayne County, Utah. September, 1936.
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Panorama with Image 458. Morning of July 10. Small flood falling into box canyon at Bert Avery Seep. Normally no water flows here except for a small seep from under the sandstone (Ferron). Wayne County, Utah. July, 1936.
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Panorama with Image 479. Horseshoe Ridge. The cliff is porphyry at the base of the Horseshoe laccolith. The floor is exposed at several places along this cliff and can be seen in the picture at the extreme left. Wayne County, Utah. July, 1936.
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Transitional contact between Ferron sandstone and underlying Mancos shale. Rabbit brush along creek. View is east across mouth of creek draining Blue Basin dome. Wayne County, Utah. July, 1936.
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Greasewood mound on alluvium near the Muddy River upward from the tip of the hammer handle is wind blown material derived from the alluvium. From the tip down is bedded alluvium. Evidently, the alluvium surface has been lowered, probably by deflation. Wayne County, Utah. 1935.
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Scarp of laminated Summerville beds capped by Morrison conglomerate and Gypsum. North side of Fremont River by Hanksville Bridge. The flood plain of the Fremont shows in foreground. Wayne County, Utah. September, 1936.
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Blue Gate shale (Mancos) of Gilbert in southern Wayne County on trail to Mount Ellen from Notom Ranch. Wayne County, Utah. 1921.
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E. Bowles at plane table by triangulation flag "Corner". Wayne County, Utah. July, 1936.
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View north across upper part of Sawmill Basin, from North Pass, Mount Ellen. Wayne County, Utah. May, 1936.
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Views in the badlands and mesa areas: Badlands in the upper part of the Ferron sandstone member of the Mancos shale, along state route 24, the highest badland hills are formed by the Blue Gate shale member of the Mancos shale. In the distance is Factory Butte. Wayne County, Utah. 1935. Figure 98-C, in U.S.Geological Survey Professional paper 228. 1953.
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The Todilto (?) formation and Wingate sandstone in Capitol Wash, southern Wayne County, Utah. The Wingate is the very massive sandstone which forms the lower canyon walls. Wayne County, Utah. 1921.
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Gravel covered pediments at the foot of Mount Ellen [Peak]: form a panorama looking south across the Dugout Creek benches; sandstone hills protrude through the gravel, which is about 25 feet thick. Wayne County, Utah. 1936. Figure 103-B, in U.S.Geological Survey Professional paper 228. 1953.
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Dakota sandstone where crossed by Highway 24. The formation consists of two sandstone and an intervening coal bearing shale unit, each about 25 feet thick. The shale and lower sandstone are cross bedded, shale bedding grading into sandstone bedding and the cross beds truncated by the top sandstone. The shale is interpreted as top set beds, the lower sandstone as foreset beds. View is nearly west. Wayne County, Utah. 1935.
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View north up Nazer Canyon to head of Canyon. Forest of aspen on west side of canyon, Douglas fir and yellow pine on east side, and spruce- fir forest at head. So far as known the rock in the canyon is porphyry. Wayne County, Utah. September, 1936.
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Hugh D. Miser, on Dolly, in aspen woods west of White Rocks Ridge. Wayne County, Utah. September, 1936.
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Panorama with Images 403 and 405. View north across Fremont at Hanksville. Conglomerate of Curtis Formation truncates an anticline in Entrada Formation. Summerville and Morrison Formations on left skyline. Wayne County, Utah. 1935.
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Northwest side of Table Mountain (Marvine laccolite). The rock is all porphyry. Facets are approximately at the outer contact for locally small masses of Mancos shale are exposed at the base. Wayne County, Utah. July, 1936.
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Views of stream channels and alluvium north of Mount Ellen [Peak]: This was the channel of the Fremont River prior to 1896. The channel, 65 feet wide and 5 ft. deep here, is part of a cut-off meander preserved in the alluvial plain where the Fremont joins the Muddy River (S 1/2 sec.3, T. 28 S., R. 11 E.) Wayne County, Utah. 1939. Figure 114- A, in U.S.Geological Survey Professional paper 228. 1953.
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The Factory Butte Coal Mine, mining an 8-foot bed of coal, has a sandstone roof properly supported here with timbers. Wayne County, Utah. 1935.
map background search result map search result map Views in the badlands and mesa areas. Wayne County, Utah. 1935. Gravel covered pediments at the foot of Mount Ellen: form a panorama looking south across the Dugout Creek benches. Wayne County, Utah. 1936. Views of stream channels and alluvium north of Mount Ellen: This was the channel of the Fremont River prior to 1896. Wayne County, Utah. 1939. Conglomerate of Curtis Formation truncates an anticline in Entrada Formation. Wayne County, Utah. 1935. The Todilto formation and Wingate sandstone in Capitol Wash. Wayne County, Utah. 1921. Conglomerate of Curtis Formation truncates an anticline in Entrada Formation. Wayne County, Utah. 1935. The Todilto formation and Wingate sandstone in Capitol Wash. Wayne County, Utah. 1921. Views in the badlands and mesa areas. Wayne County, Utah. 1935. Gravel covered pediments at the foot of Mount Ellen: form a panorama looking south across the Dugout Creek benches. Wayne County, Utah. 1936. Views of stream channels and alluvium north of Mount Ellen: This was the channel of the Fremont River prior to 1896. Wayne County, Utah. 1939.