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TitleDateTypeSetname
76 Amalga Barrens and Cutler Reservoir, Utah [04]2001-11-07; 2001-11-08; 2001-11-09uum_map
77 Amalga Barrens and Cutler Reservoir, Utah [05]2001-11-07; 2001-11-08; 2001-11-09uum_map
78 Amalga Barrens and Cutler Reservoir, Utah [06]2001-11-07; 2001-11-08; 2001-11-09uum_map
79 Amalga Barrens and Cutler Reservoir, Utah [07]2001-11-07; 2001-11-08; 2001-11-09uum_map
80 Amalga Barrens and Cutler Reservoir, Utah [08]2001-11-07; 2001-11-08; 2001-11-09uum_map
81 Amalga Barrens and Cutler Reservoir, Utah [09]2001-11-07; 2001-11-08; 2001-11-09uum_map
82 Amalga Barrens and Cutler Reservoir, Utah [10]2001-11-07; 2001-11-08; 2001-11-09uum_map
83 Amalga Barrens and Cutler Reservoir, Utah [11]2001-11-07; 2001-11-08; 2001-11-09uum_map
84 Amalga Barrens and Cutler Reservoir, Utah [12]2001-11-07; 2001-11-08; 2001-11-09uum_map
85 Amalga Barrens and Cutler Reservoir, Utah [13]2001-11-07; 2001-11-08; 2001-11-09uum_map
86 Amalga Barrens and Cutler Reservoir, Utah [14]2001-11-07; 2001-11-08; 2001-11-09uum_map
87 Amalga Barrens and Cutler Reservoir, Utah [15]2001-11-07; 2001-11-08; 2001-11-09uum_map
88 The ancient Green River carved deep rock whirlpools in the side of Lodore Canyon1955uum_map_rr
89 Ancient landslides show up on maps with scales as small as one inch to the mile. Three such ancient slides are pointed out along the mountain front in Juab County. Note swath of anomalous contours leading down to lowermost slide, obviously the path of bedrock which failed.Imageuum_map
90 Andy Hetzel snowboarding at Crested Butte, CO.1998uum_map_usa
91 Another example of dynamic forces at work in the geologic environment: pressure ridges formed in the salt crust of Utah's Bonneville Salt Flats. These ridges grow and shrink seasonally.Imageuum_map
92 Approaching 1st lunch stop. 6-11-551955-06-11Imageuum_map_rr
93 Approaching Flaming Gorge1955uum_map_rr
94 Approaching Flaming Gorge. Susp[ension] bridge. 6-11-55 [sic]1955-06-11Imageuum_map_rr
95 Areas of carbonate rock (limestone) outcrops (in blue) in the vicinity of Bear Lake, Utah. Rocks range in age from Cambrian to Jurassic. Development on the outcrop area should be closely monitored to protect the underlying potable water aquifer.Imageuum_map
96 Arizona waters, April 9, 19481948-04-09Image/StillImageuum_map
97 Arrow points to incipient failure of an excavation wall for a foundation for a multistory office building. Material is horizontally stratified Lake Bonneville silts and sands.Imageuum_map
98 Ashley Falls. 6-13-551955-06-13Imageuum_map_rr
99 At House Rock, Marble Canyon1956uum_map_rr
100 At Lee's Ferry, April 10, 1948 [01]1948-04-10Image/StillImageuum_map
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