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Death Valley National Park, California. Tubular orifices in the fine sediments at Salt Springs near the north side of Borax Camp allow discharge of water to the valley floor. Light areas are accumulations of salts from previous discharges. Circa 1960. Figure 10, U.S. Geological Survey Professional paper 494-B.
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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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Looking south from Cerro de Los Cuates, the mesa across the Rio Puerco is capped with Cretaceous sandstone. Sandoval County, New Mexico. 1930. Plate 12-C, U.S. Geological Survey Professional paper 189B. 1938. Album caption: View S. from the top of Cerro de Los Cuates. Sandoval Co., New Mexico [1932]
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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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Panorama with Image 666. View south across Trachyte Creek from northeast corner of section 1, township 33 south, range 12 east. Mount Holmes and Mount Ellsworth on right skyline. Carmel formation on Navajo sandstone in foreground. Garfield County, Utah. September, 1937.
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Gravel covered pediments at the foot of Mount Ellen [Peak]: Form a panoramic view northeast across the dissected north edge of the Birch Creek Benches. The gravel is 6 to 10 feet thick and lies on a pediment eroded in Tununk shale member of the Mancos shale. Garfield County, Utah. July 1936. Figure 103-A, in U.S.Geological Survey Professional paper 228. 1953.
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Death Valley National Park, California. Burro Trail fault on the south side of Trail Canyon. Nopah Formation in the upper plate lies almost horizontally on the almost horizontal thrust fault. The lower plate is Bonanza King Formation. Circa 1960. Figure 116, U.S. Geological Survey Professional paper 494-A.
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Desert holly (Atriplex hymenelytra),the most drought resistant shrub in Death Valley. The ash of the leaves contains 30 to 35 percent of sodium chloride. Death Valley National Park. Inyo County, California. ca. 1960. (Photo by J. R. Stacy)
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Death Valley National Park, California. Furnace Creek Formation at the north end of the Black Mountains. View is southwest and west of Zabriskie Point, an overlook by Highway 190 about 3 miles up Furnace Creek Wash from Furnace Creek Inn. The base of the Furnace Creek Formation is at the topographic break between the badlands and the rougher, higher ground in the distance on the left. Light-colored playa beds about 2,500 feet thick extend to the base of a conglomerate which forms the dark cliff at the right. The beds are dipping to the right (north) into the Texas Spring Syncline. The center of the photograph looks west across Death Valley to the Panamint Range at Aguereberry Point; Tucki Mountain on the right....
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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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Views on Mount Ellen Peak: The floor of the South Creek laccolith at the west end of South Creek Ridge. The porphyry rests on carbonaceous shale and sandstone in the upper part of the Ferron sandstone member of the Mancos shale. Garfield County, Utah. May 1937. Figure 25-C, in U.S.Geological Survey Professional paper 228. 1953.
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Cross section of basaltic next exposed by erosion in Grant Ridges, 6 miles northeast of Grant, view looking southwest in sec. 3, T. 11 S., R. 9 W. Basalt in core is jointed in vertical columns and surrounded by a thin zone of platy jointing developed along the contact with white tuff. Bedded breccia overlies the tuff, and basaltic lava overlies the breccia on the far side of the cone. The tuff, chiefly rhyolitic, was erupted from Mount Taylor. Valencia County, New Mexico. 1931. Plate 11-A, U.S.Geological Survey Professional paper 189-B. 1938. Album: Hunt #62, Valencia County, New Mexcio, 1931. T. 11 S., R. 9 W, Sec. 3 View NW. at natural cross-section of a cinder cone 6 miles northeast of Grant. Columnar jointed...
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Thin section of diorite porphyry, from sill beneath the Copper Ridge laccolith; the lower part of the section is a hornblendic inclusion containing the same plagioclase and hornblende as the diorite porphyry. X 6. Garfield County, Utah. 1939. Figure 80-C, in U.S.Geological Survey Professional paper 228. 1953.
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Canyon views: Northwest across the Colorado River just below Dandy Crossing; Indian ruins in right foreground. San Juan County, Utah. 1939. Figure 9-B, with graphics, in U.S.Geological Survey Professional paper 228. 1953.
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Death Valley National Park, California. Burial mounds are numerous on the gravel fans near the Death Valley III and Death Valley IV sites. This was identified as a Death Valley IV mound; the Death Valley III ones are similar. Circa 1960.
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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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Death Valley National Park, California. Noonday Dolomite, showing structures of Scolithus tubes at the east foot of the mountain at the spur south of Galena Canyon. Circa 1960. Figure 9, U.S. Geological Survey Professional paper 494-A.
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Death Valley National Park, California. Dowels set on terracettes showed virtually no movement in several years. The terracettes seem to be stable in the present climate. They probably formed at a time when the climate was wetter, as it must have been at the time of the Holocene lake on the floor of Death Valley. Circa 1960.
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Death Valley National Park, California. Bioclastic bed with fragments of trilobites and brachiopods from shale unit at the base of the Nopah Formation. Circa 1960. Figure 23, U.S. Geological Survey Professional paper 494-A.
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Death Valley National Park, California. Amphipora(?) beds are abundant in the middle of the Lost Burro Formation. Circa 1960. Figure 30 (lower photo), U.S. Geological Survey Professional paper 494-A.
map background search result map search result map Cross section of basaltic next exposed by erosion in Grant Ridges. Valencia County, New Mexico. 1931. Looking south from Cerro de Los Cuates. Sandoval County, New Mexico. 1930 Views in the badlands and mesa areas. Wayne County, Utah. 1935. Gravel covered pediments at the foot of Mount Ellen. Garfield County, Utah. 1936. Gravel covered pediments at the foot of Mount Ellen: form a panorama looking south across the Dugout Creek benches. Wayne County, Utah. 1936. Views on Mount Ellen Peak: The floor of the South Creek laccolith at the west end of South Creek Ridge. Garfield County, Utah. 1937. 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. Canyon views: Northwest across the Colorado River just below Dandy Crossing; Indian ruins in right foreground. San Juan County, Utah. 1939. Thin section of diorite porphyry, from sill beneath the Copper Ridge laccolith. Garfield County, Utah. 1939. Death Valley National Park, California. Noonday Dolomite, showing structures of Scolithus tubes at the east foot of the mountain at the spur south of Galena Canyon. Circa 1960. Bioclastic bed with fragments of trilobites and brachiopods from shale unit at the base of the Nopah Formation. Death Valley National Park, California. 1960. Amphipora(?) beds are abundant in the middle of the Lost Burro Formation. Death Valley National Park, California. 1960. Burro Trail fault on the south side of Trail Canyon. Death Valley National Park, California. 1960. Death Valley National Park, California. Tubular orifices in the fine sediments at Salt Springs near the north side of Borax Camp allow discharge of water to the valley floor. Circa 1960. Death Valley National Park, California. Dowels set on terracettes showed virtually no movement in several years. Circa 1960. Death Valley National Park, California. Burial mounds are numerous on the gravel fans near the Death Valley III and Death Valley IV sites. Circa 1960. Desert holly (Atriplex hymenelytra),the most drought resistant shrub in Death Valley. The ash of the leaves contains 30 to 35 percent of sodium chloride. ca. 1960. Furnace Creek Formation at the north end of the Black Mountains. Death Valley National Park, California. 1960. Conglomerate of Curtis Formation truncates an anticline in Entrada Formation. Wayne County, Utah. 1935. View south across Trachyte Creek from northeast corner of section 1, township 33 south, range 12 east. Garfield County, Utah. 1937. Cross section of basaltic next exposed by erosion in Grant Ridges. Valencia County, New Mexico. 1931. Conglomerate of Curtis Formation truncates an anticline in Entrada Formation. Wayne County, Utah. 1935. Looking south from Cerro de Los Cuates. Sandoval County, New Mexico. 1930 View south across Trachyte Creek from northeast corner of section 1, township 33 south, range 12 east. Garfield County, Utah. 1937. Death Valley National Park, California. Noonday Dolomite, showing structures of Scolithus tubes at the east foot of the mountain at the spur south of Galena Canyon. Circa 1960. Bioclastic bed with fragments of trilobites and brachiopods from shale unit at the base of the Nopah Formation. Death Valley National Park, California. 1960. Amphipora(?) beds are abundant in the middle of the Lost Burro Formation. Death Valley National Park, California. 1960. Burro Trail fault on the south side of Trail Canyon. Death Valley National Park, California. 1960. Death Valley National Park, California. Tubular orifices in the fine sediments at Salt Springs near the north side of Borax Camp allow discharge of water to the valley floor. Circa 1960. Death Valley National Park, California. Dowels set on terracettes showed virtually no movement in several years. Circa 1960. Death Valley National Park, California. Burial mounds are numerous on the gravel fans near the Death Valley III and Death Valley IV sites. Circa 1960. Desert holly (Atriplex hymenelytra),the most drought resistant shrub in Death Valley. The ash of the leaves contains 30 to 35 percent of sodium chloride. ca. 1960. Furnace Creek Formation at the north end of the Black Mountains. Death Valley National Park, California. 1960. Canyon views: Northwest across the Colorado River just below Dandy Crossing; Indian ruins in right foreground. San Juan County, Utah. 1939. Views in the badlands and mesa areas. Wayne County, Utah. 1935. Gravel covered pediments at the foot of Mount Ellen. Garfield County, Utah. 1936. Gravel covered pediments at the foot of Mount Ellen: form a panorama looking south across the Dugout Creek benches. Wayne County, Utah. 1936. Views on Mount Ellen Peak: The floor of the South Creek laccolith at the west end of South Creek Ridge. Garfield County, Utah. 1937. 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. Thin section of diorite porphyry, from sill beneath the Copper Ridge laccolith. Garfield County, Utah. 1939.