Photo Archives
 
Filters: Collection Name: "Herbert E. Gregory" Date: "1944" Format: "application/pdf"
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1 Bowers Knoll; Volcano viewed from northwest. Garfield County, UT. 19441944Image
2 Brian Head formation, branch of Asay Creek; lies beneath basalt flows. Garfield County, UT, 19441944Image
3 East side of Lone Rock on Wah Weap Creek1943; 1944; 1945Image
4 End of lava flow 6 miles long in Black Creek Valley1943; 1944; 1945Image
5 Eroded flank of the East Kaibab monocline at the junction of Paria River and Cottonwood Creek (left center). The sequence is Navajo (left), upper Jurassic (largely eroded), Dakota, Tropic, and Straight Cliffs. Kane County, UT, 19441944Image
6 Features of the East Kaibab monocline [and] Structural relations of rocks along Utah-Arizona boundary1943; 1944; 1945Image
7 Flat lying Upper Jurassic (foreground) and Cretaceous strata bed abruptly upward against the Navajo on the flank of the East Kaibab monocline (left sky line). Table Cliffs (right sky line) is about 50 miles north. Paria Valley near Adairville. Kane County, UT. 19441944Image
8 Herbert E. Gregory Book 12: Colorado Plateau, Province, 1942-19441942; 1943; 1944Image
9 Hillside of eroded rock, Paria Valley, Utah1943; 1944; 1945Image
10 Kaibab limestone (lower wall,left, breccia (marks unconformable contact), and basal Moenkopi limestone and shales. Mouth of Kaibab Gulch. Kane County, UT, 19441944Image
11 Lava, Black Rock Valley1943; 1944; 1945Image
12 Looking south (up dip) down the Paria River, which has widened its floor and dissected its borders in Upper Jurassic rocks (foreground) and cut a deep narrow canyon in the Navajo sandstone (background). Site of the abandoned Adairville. Kane County UT, 19441944Image
13 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
14 Looking south, up dip, across West Clark Bench, Upper Jurassic and Dakota (butte), to the Paria Terrace, Navajo sandstone. Paria River, which passes through 'The Gap' is joined by Kaibab Creek. Kane County, UT. 19441944Image
15 Mesa capped by Dakota sandstone eroded from upper Jurassic Winsor (?) formation. Head of Ash Creek. Kane County, UT1944Image
16 Mound of sedimentary material, vicinity of Paria River, Utah1943; 1944; 1945Image
17 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
18 Panorama--4 photographs. Blue Springs meadows. A former valley leading to Mammoth Creek blocked by basalts from Miller Knoll (right skyline) became a lake that eventually cut an outlet northward through the Brian Head formation (upper left). Garfield County, UT, 19441944Image
19 Paria Canyon, Utah1943; 1944; 1945Image
20 Paria Valley and east flank of East Kaibab monocline1943; 1944; 1945Image
21 Road and lava field, Rock Creek Valley, Utah1943; 1944; 1945Image
22 Rocky cliff near Hillsdale1943; 1944; 1945Image
23 Sandstone outcrops, Paria Canyon, Utah1943; 1944; 1945Image
24 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
25 Sevier River formation overlaid by basalt near mouth of Corral Creek on Highway 89, 2 miles east of Panguitch. Garfield County, UT. 19441944Image
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