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1 Looking across Big Plains toward Smithsonian Butte (middle background), West Temple (upper right). Foreground forested east slope of Little Creek Mountain, Shinarump; middle distance, dry farm lands on Chinle strata. Washington County, Utah, 1937.1937Image
2 Looking southward across House Rock Valley from West Clark Bench. West dipping Navajo sandstone trenched by Kaibab Creek (middle distance) is a part of the East Kaibab monocline; east dipping limestones (skyline) are the cap rocks of the Kaibab upwarp. Kane County, UT, 19441944Image
3 Water Pocket Fold. East entrance to Muley Twist Trail. Wingate and Middle LaPlata. Kane County, UT. June 19181918Image
4 Looking east across Sevier River near Hatch River terraces in middle distance, "Pink Cliffs" (Wasatch) in background bounded by Sevier fault. Garfield County, Utah, 1936.1936Image
5 Looking northwest across Parunuweap east of Mt. Carmel, Cretaceous in middle ground, Pink Cliffs in distance, 1936.1936Image
6 Moenkopi formation: Shnabkaib member (lower part), upper red sandstone (upper middle), Shinarump conglomerate (top). East side of Seamans Wash, Kane County, UT. 19431943Image
7 Keet Seel, cliff ruins east middle branch of Sagy (Towanaoche) canyon, Ariz., 1910 (Photo G165)1910Image
8 Section of the Shinarump Cliffs (middle distance), east of Pioneer Gap. Shinarump conglomerate exposed by erosion of Moenkopi formation below and the basal strata of the Chinle formation above. Upper Chinle sandstones form Vermilion Cliffs (background).1944Image
9 View looking east across Parunuweap Valley near Mt. Carmel. Distance Elkheart Cliffs (Navajo capped by Carmel) on upthrown side of Sevier fault; middle distance erosion surface in Carmel and other Jurassic. Kane County, Utah, 1932.1934Image
10 Looking down Notch Canyon from East Point, Elk Ridge, toward Chimney Park. Cottonwood Canyon in middle distance. Buttes of Navajo beyond Shay Mountains in distance. San Juan County, UT, 1928Image
11 Looking down Notch Canyon from East Point, Elk Ridge, toward Chimney Park. Cottonwood Canyon in middle distance. Buttes of Navajo beyond Shay Mountains in distance. San Juan County, UT, 19281928Image
12 Panorama {a}. Flank of East Kaibab monocline, bordering alluvial floor of Paria Valley. Navajo sandstone (middle sky line), Upper Jurassic strata, and basal Cretaceous (left). Dips of 40 degrees decrease to 3 degrees within 1,000 feet. Kane County, UT, 19441944Image
13 Panorama {b}. Flank of East Kaibab monocline, bordering alluvial floor of Paria Valley. Navajo sandstone (middle sky line), Upper Jurassic strata, and basal Cretaceous (left). Dips of 40 degrees decrease to 3 degrees within 1,000 feet. Kane County, UT, 19441944Image
14 Panorama {c}. Flank of East Kaibab monocline, bordering alluvial floor of Paria Valley. Navajo sandstone (middle sky line), Upper Jurassic strata, and basal Cretaceous (left). Dips of 40 degrees decrease to 3 degrees within 1,000 feet. Kane County, UT, 19441944Image
15 Panorama {d}. Flank of East Kaibab monocline, bordering alluvial floor of Paria Valley. Navajo sandstone (middle sky line), Upper Jurassic strata, and basal Cretaceous (left). Dips of 40 degrees decrease to 3 degrees within 1,000 feet. Kane County, UT, 19441944Image
16 View looking northeast across Kolob Terrace. Basalt (foreground), Cretaceous trenched by Crystal Creek (middle), Pink Cliffs-Wasatch (skyline), lower east slope of Black Mountain (extreme left), 'The Gap,' twin peaks (right skyline), stands just south of Navajo Lake. Iron County, UT, 19421942Image
17 Looking west across Panguitch. Sevier River formation (foreground), alluvium (middle distance), basalt (left center), and pyroclastic slopes leading to Little Creek Peak (background), on the east wall of Bear Valley. Garfield County, UT, 19441944Image
18 Panorama {c}. Flank of East Kaibab monocline, bordering alluvial floor of Paria Valley. Navajo sandstone (middle sky line), Upper Jurassic strata, and basal Cretaceous (left). Dips of 40 degrees decrease to 3 degrees within 1,000 feet. Kane County, UT, 19441944Image
19 Panorama {e}. Flank of East Kaibab monocline, bordering alluvial floor of Paria Valley. Navajo sandstone (middle sky line), Upper Jurassic strata, and basal Cretaceous (left). Dips of 40 degrees decrease to 3 degrees within 1,000 feet. Kane County, UT, 19441944Image
20 View looking east across north end of No Man's Mesa, composed of Navajo sandstone partly capped by Carmel limestone. Park Wash (foreground) area drained by Kitchen Canyon tributary to Paria River (middle background). Panoramic with no. 887. Kane County, UT, 19401940Image
21 Zion Park Cliffs, from Shinarump bench, near base of Smithsonian Butte. Virgin River in middle distance; West Temple center distance; at the right Bridge Mountain, East Temple, The Twin Brothers, and Mountain of the Sun. Zion National Park, Utah, 1936.1936Image
22 Looking south along Paria River from the mouth of Shurtz Gorge. Navajo sandstone in East Kaibab monocline is overlaid with decreasing dips by Upper Jurassic (banked against the Navajo), Dakota, and Tropic (foreground and left sky line). Erosion surface (middle distance) bevels upturned rocks. Kane County, UT, 19441944Image
23 Looking south along Paria River from the mouth of Shurtz Gorge. Navajo sandstone in East Kaibab monocline is overlaid with decreasing dips by Upper Jurassic (banked against the Navajo), Dakota, and Tropic (foreground and left sky line). Erosion surface (middle distance) bevels upturned rocks. Kane County, UT, 19441944Image
24 Looking N 80° E at the head of To-Chin-Sin canyon. Pastora Peak in right background. Cliffs through middle ground are monzonite porphyry.1913Image
25 Butte, junction Sagy canyon with middle of East Branch, Ariz., 1910 (Photo G162)1910Image
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