. Bulletin of the Geological Society of America. Geology. 296 S. P. EMMONS UINTA MOUNTAINS the generally low angle at which the beds stand and the peculiar topo- graphic forms, the true succession of the respective exposures is often. ^F ContoTiT Intexval 100 feet. LEGEND 7777 'ZA WEBER QUARTZITE WASATCH LIMESTONE OSOEN QUARTZITE SHALE SERIES UINTA QUART2ITE Figure 2.—Geological Sketch Map of Duchesne Canyon Region, Western Uinta Mountains. difficult to determine. The lithologic constitution of the beds has suf- fered a remarkable change from the Wasatch section, considering the short distance
. Bulletin of the Geological Society of America. Geology. 296 S. P. EMMONS UINTA MOUNTAINS the generally low angle at which the beds stand and the peculiar topo- graphic forms, the true succession of the respective exposures is often. ^F ContoTiT Intexval 100 feet. LEGEND 7777 'ZA WEBER QUARTZITE WASATCH LIMESTONE OSOEN QUARTZITE SHALE SERIES UINTA QUART2ITE Figure 2.—Geological Sketch Map of Duchesne Canyon Region, Western Uinta Mountains. difficult to determine. The lithologic constitution of the beds has suf- fered a remarkable change from the Wasatch section, considering the short distance that separates Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original Geological Society of America. [New York : The Society]
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Keywords: ., bookcentury1800, bookdecade1890, booksubjectgeology, bookyear1890
