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View down the North Wash fan from road. Garfield County, Utah. September, 1937.
Panorama with Images 531, 532, 533, and 534. View down the canyon of the Fremont River from north rim of mouth of Poison Box Canyon. The light beds along the river are Permian; Moenkopi formation forms slope below light ledge which is Shinarump. Chinle formation forms slope up to big cliff which is Wingate. Ledges of sandstone above the Wingate are Kayenta and light massive sandstone above Kayenta is Navajo. Photo by R.L. Miller. Wayne County, Utah. September, 1936.
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.
Panorama with Images 696 and 698. View west up South Fork across north flank of the dome to Copper Ridge laccolith. Garfield County, Utah. September, 1937.
Panorama with Images 685, 687, 688, and 689. Panorama with southwest- northwest from the Morrison Reef, three-fourths mile south of South Fork. Wingate, Kayenta, and Navajo are exposed in this dome. Beyond this dome is Ragged Mountain (bysmalith) and the Copper Ridge laccolith. The butte at right is Bull Mountain - also a bysmalith. Garfield County, Utah. September, 1937.
View north along Church Street. Hanksville, Utah. Garfield County, Utah. September, 1938.
View northwest across the head of Brown Creek. Pennell Peak in the distance. Garfield County, Utah. September, 1938.
Panorama with Image 661. Talus cone at the lake on north side of Bulldog Peak. Garfield County, Utah. August, 1937.
View is north at north rim of Bromide Basin. The scars are rock slides. Garfield County, Utah. June, 1937.
Porphyry sill exposed on north side of South Creek. Garfield County, Utah. May, 1937.
View southwest at the southwest rim of the Bromide Basin. Garfield County, Utah. June, 1937.
Panorama with Image 418. Snow capped Mount Ellen with gravel capped erosion surfaces in foreground. View is west from Poison Spring bench by road to Trachyte Ranch. Garfield County, Utah. April, 1936.
Panorama with Image 432. East side summit ridge of Mount Ellsworth. Jagged porphyry dikes intrude vitropyre which forms slopes. Ellsworth spike camp at saddle in upper left. Garfield County, Utah. April, 1936.
View up Cedar Creek from south side near mouth. Cedar Creek Stock exposed on north side of creek. The dome in the Morrison beds in the pinyon-juniper woods is produced by the north edge of the Shoulder laccolith. These northward dipping beds are intruded discordantly by the Cedar Creek Stock. Wayne County, Utah. September, 1936.
Panorama with Image 457. 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.
Fragments of bioclastic "trilobite- trash" bed typical of the lower part of the Carrara Formation. The trilobites are olenellids. Death Valley National Park, California. Circa 1960. Figure 19, U.S. Geological Survey Professional Paper 494-A.
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Panorama with Image 575. (1) Laccolithic ridges. (2) View north across Dugout from Little Ragged Butte. Corral Ridge laccolith forms conspicuous round hill in center. North Summit Ridge at right and Shoulder laccolith at left. Garfield County, Utah. June, 1937.
View along the northeast side of Table Mountain (Marvine laccolith). The porphyry intrusion forms the cliff with talus slope at the right. In the center and left is Ferron sandstone turned up by the intrusion. Wayne County, Utah. September, 1936.
View is north from upper part of Straight Creek gravel bench; shows Ragged Mountain at extreme left and the arch east of it. Bull Mountain on left skyline. Garfield County, Utah. July, 1937.
Six huge monoliths at the north side of Table Mountain (Marvine laccolite). These monoliths are porphyry and represent that part of the intrusion that contacted the country rock. The interior has been eroded but these remain. Their greater resistance to erosion is probably controlled by jointing for the rock at the contact differs only very slightly from rock in the interior of the intrusion. Wayne County, Utah. July, 1936.
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