. Bulletin of the Geological Society of America. Geology; Geology -- United States. FiauEE 6.âEastern Slop< of Mount Jura. I Hinchman tuil : 5 â Bicknell sandstom G Mormon sandstone; 7 Thompson limestone; 8 = Illiniumvi' sandstone; E= Eruptive rocks. grave sandstone, Thompson limestone and Mormon sandstone are re- peated in exactly the same order on opposite slopes, as represented in figure â¢'). Such a repetition ofthe strata can be produced only by faulting. ftformon Canon of Indian Creek Mt. Jura Hi nchman rav I no. Pioi kjb 6.âSection through Mount Jura. 4 = Hinchman tuff; 5 = Bick
. Bulletin of the Geological Society of America. Geology; Geology -- United States. FiauEE 6.âEastern Slop< of Mount Jura. I Hinchman tuil : 5 â Bicknell sandstom G Mormon sandstone; 7 Thompson limestone; 8 = Illiniumvi' sandstone; E= Eruptive rocks. grave sandstone, Thompson limestone and Mormon sandstone are re- peated in exactly the same order on opposite slopes, as represented in figure â¢'). Such a repetition ofthe strata can be produced only by faulting. ftformon Canon of Indian Creek Mt. Jura Hi nchman rav I no. Pioi kjb 6.âSection through Mount Jura. 4 = Hinchman tuff; 5 = Bicknell sandstone; 6= = Mormon sandstone; 7 Thompson lime 8 Hardgrave sandstone; 9 Foreman beds; LI = Hosselkus limestone; E = Eruptive rocks. We should expect the fault or its attendant phenomena to hi' displayed on the western 'slope of mount Jura, where the repetition begins, and in fact we find at that point a number of exposure- deserving special men- tion. ,*-"-5C- Fioubk 7. -<S I'l'-' a ' â nerwirtlCs ⢠Mormon sandstone; 7 Th pson limesl ; 8 Hardgrave sandstone; E Eruptive rocks. On the second prominent spur, which reaches the stage road south of the Indian village at an elevation of 5,100 feet, an outcrop nearly LOO fei'i in length is exposed. It is illustrated in figure 7. LI l-l'.ri i flKOi Soi . \\ Vol . ::. 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, etc. ] The Society
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