Photo Archives
 
Filters: Date: "1944" Collection: "uum_map"
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TitleCollection Number And NamePhoto Number
1 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, 1944P0013 Herbert E. Gregory Photograph CollectionP0013n12_035_2882
2 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).P0013 Herbert E. Gregory Photograph CollectionP0013n12_052B
3 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, 1944P0013 Herbert E. Gregory Photograph CollectionP0013n12_042_2889
4 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, 1944P0013 Herbert E. Gregory Photograph CollectionP0013n12_042_2890
5 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, 1944P0013 Herbert E. Gregory Photograph CollectionP0013n12_042_2891
6 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, 1944P0013 Herbert E. Gregory Photograph CollectionP0013n12_043_2892
7 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, 1944P0013 Herbert E. Gregory Photograph CollectionP0013n12_065_2923
8 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, 1944P0013 Herbert E. Gregory Photograph CollectionP0013n12_042_2891
9 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, 1944P0013 Herbert E. Gregory Photograph CollectionP0013n12_043_2893
10 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, 1944P0013 Herbert E. Gregory Photograph CollectionP0013n12_041_2888
11 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, 1944P0013 Herbert E. Gregory Photograph CollectionP0013n12_041_2888
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