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 them. 



