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Ledge of massive sandstone in the Carmel formation bout 150 feet above the base: on the Paria River 6 miles below Cannonville. Kane County, Utah. 1930. Plate 16-A, in U.S. Geological Survey. Professional paper 183. 1936.
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Utah Professional Paper 183,
A thin lens of limestone near the top of the Navajo sandstone in the Green River desert; locality 3 miles northeast of the junction of the Spur and Trail Spring Forks of the Horseshoe Canyon. The Carmel formation crops out on the broad bench and the Entrada sandstone forms of the cliffs in the background. Wayne County, Utah. 1931. Plate 11-A, in U.S. Geological Survey. Professional paper 183. 1936.
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Utah Professional Paper 183,
Sandstone ledges and slopes of the lower part of the Kayenta formation at Big Hole, on the Colorado River 8 miles east of Cisco. The top of the cliff formed by the Wingate sandstone is shown toward the left at the bottom of the picture. Grand County, Utah. November 1927. Plate 8-A, in U.S. Geological Survey. Professional paper 183. Plate 10-B, in U.S. Geological Survey. Bulletin 863, 1935.
Irregular contact between the Carmel formation and overlying Entrada sandstone, on the San Rafael River in sec. 14, T. 24 S., R. 15 E. Emery County, Utah. 1930. Plate 16-B, in U.S. Geological Survey. Professional paper 183. 1936.
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Utah Professional Paper 183,
Water laid bed of nodular weathering silty red sandstone near the top of the Navajo sandstone; locality is 15 miles southeast of Moab, at the southeast corner of sec. 11, T. 28 S., R. 22 E. San Juan County, Utah. 1926. Plate 15-A, U.S. Geological Survey. Professional paper 183. 1936.
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photo print
Banded shale in the upper part of the Morrison formation, 13 miles southwest of Green River, along the road from Green River to Hanksville. The ledge at the top of the slope is formed by a bed of siliceous sandstone near the top of the formation. Emery County, Utah. 1930. Plate 23-C, U.S.Geological Survey Professional paper 183. 1936.
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Masses of chert weathered from the Summerville formation on Hatch Rock, sec. 1, T. 30 S. R. 22 E., photo by L.W. Clark. San Juan County, Utah. 1927. Plate 22-D, U.S.Geological Survey Professional paper 183. 1936.
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Intricate cross bedding in the Entrada sandstone, in the northern part of sec. 5, T. 21 S., R. 23 E., about 8 miles northeast of Cisco; the white sandstone at the top is the lower part of the Moab sandstone member. Grand County, Utah. November 1927. Plate 18-D, in U.S. Geological Survey. Professional paper 183. Plate 14-A, in U.S. Geological Survey. Bulletin 863, 1935.
Entrada sandstone and lower part of the Morrison formation near the mouth of Cottonwood Wash, Bluff; the low ledge in the foreground represents the complete thickness of the Entrada sandstone near the southern limit of the formation. The slope forming beds and the massive ledge of sandstone ("Bluff sandstone") make up the lower part of the Morrison formation. San Juan County, Utah. 1925. Plate 19-A, in U.S. Geological Survey. Professional paper 183. 1936.
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Utah Professional Paper 183,
Tangential cross-bedding in the upper part of the Navajo sandstone in Dry Valley, sec. 9, T. 30 S., R.23 E., 26 miles north of Monticello. San Juan County, Utah. 1925. Plate 15- C, in U.S. Geological Survey. Professional paper 183. 1936.
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Utah Professional Paper 183,
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Outcrop of the Carmel formation in a fork of Moonshine Canyon in sec. 20, T. 24 S., R. 16 E., Green River desert; the tanks in foreground rest on the Navajo sandstone, which is overlain by the limy sandstone beds at the base of the Carmel formation. Gypsiferous shale and sandstone beds of the Carmel formation form the upper part of the canyon wall. Emery County, Utah. 1930. Plate 15-B, U.S. Geological Survey. Professional paper 183. 1936.
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Utah Professional Paper 183,
Solution pits in the Entrada sandstone about 1 mile southeast of Cane Springs, the Moab sandstone member at the top of the Entrada sandstone is overlain by the Summerville formation and Morrison formation. San Juan County, Utah. 1930. Plate 17-C, with graphics, in U.S. Geological Survey. Professional paper 183. 1936.
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Utah Professional Paper 183,
Wingate sandstone and underlying softer Chinle shale exposed at Big Hole on the Colorado River 8 miles east of Cisco, note the extensive horizontal softer beds in the Wingate sandstone and the cross-bedding within the thicker sandstone beds. sec. 8 T. 21 S., R. 23 E. Grand County, Utah. October 1927. Plate 6-B, in U.S. Geological Survey. Professional paper 183. 1936. Plate 9-A, in U.S. Geological Survey. Bulletin 863, 1935.
Irregular bedding in the massive Entrada sandstone, about 8 miles east of Flattop Buttes in the Green River desert. Emery County, Utah. 1931. Plate 17-A, in U.S. Geological Survey. Professional paper 183. 1936.
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Utah Professional Paper 183,
photo print
Indefinite contact between the Kayenta formation and the overlying Navajo sandstone, on the west bank of the Colorado River at the mouth of (now Negro Bill) Creek, in sec. 19, T. 25 S., R. 22 E. Grand County, Utah. 1926. Plate 8-C, in U.S. Geological Survey. Professional paper 183. 1936.
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Utah Professional Paper 183,
Intraformational unconformity about 50 feet below the top of the Kayenta formation on the east side of Cottonwood Canyon; sec. 2 T. 32 S., R. 21 E., photo by L.W. Clark, San Juan County, Utah. 1927. Plate 8-B, in U.S. Geological Survey. Professional paper 183. 1936.
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Tags: Baker, A.A. Collection,
Formations,
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Utah Professional Paper 183,
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