. Bulletin of the Geological Society of America. Geology. I inch = 4feet. / inch =â 8feet. FiGUiiE il. âContact lyrokcn by a Thrust Fault. FuaiiE -IS.âContact broken bij a Gravity Fault. Entering Williams canyon at the lower (southern) end, we pass between walls of the Manitou limestone; the glauconitic red sandstone (Cambrian) first appears at the Narrows, about half a mile from the mouth of the â Figure 29.âOverthrust Flexure of the banal Cambrian Beds in Fourth Outlier. canyon ; between two and three hundred feet beyond this we strike the top of the basal gray sandstone, and about
. Bulletin of the Geological Society of America. Geology. I inch = 4feet. / inch =â 8feet. FiGUiiE il. âContact lyrokcn by a Thrust Fault. FuaiiE -IS.âContact broken bij a Gravity Fault. Entering Williams canyon at the lower (southern) end, we pass between walls of the Manitou limestone; the glauconitic red sandstone (Cambrian) first appears at the Narrows, about half a mile from the mouth of the â Figure 29.âOverthrust Flexure of the banal Cambrian Beds in Fourth Outlier. canyon ; between two and three hundred feet beyond this we strike the top of the basal gray sandstone, and about the same distance farther brings us to the granite. The general or normal dip of the strata is about south-. 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
