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Extra info for The World of Interiors - March 2012
This fold, and the next fold just downstream (fig. 28), are part of the Monument fault system. 7 m). Tapeats Sandstone, draped over the fault, dips upstream. Vishnu Schist exposed at river level downstream. 6) Royal Arch Creek (Elves Chasm), on left, is cut through a deposit of travertine that extends from the Tapeats Sandstone near river level to the top of the Muav Limestone. View of complete section of Cambrian Tonto Group and overlying strata up and including the Redwall Limestone in amphitheater to the west of Elves Chasm and a curious channel-like feature can be seen at about the level of the Temple Butte Limestone (Fonnation) in the back of the amphitheater.
View downstream of tilted cliff-forming Shinumo Quartzite (Unkar Group) unconformably overlain by basal Paleozoic strata (fig. 27). 4 m) drop. 6 kIn) above Bass Camp; Bass Limestone (Unkar Group) appears beneath Cambrian Tapeats Sandstone on right, then on left View down river to Vishnu Schist overlain by Bass Limestone that is in turn intruded by diabase sill in middle distance and on left; light colored rocks are thennally altered and bleached Bass Limestone. Above the bleached zone are ledges of the upper Bass Limestone, slope-forming red Hakatai Shale, and cliff-forming Shinumo Quartzite (extending to top of third cliff, characterized by smooth face and capped with uppennost quartzite bed of Shinumo).
The cave contains Pleistocene giant-sloth dung deposits, 11,000 to more than 40,000 years old. 7) Muddy Creek Formation (late Miocene) accumulated against Cambrian to Mississippian strata along the Grand Wash Cliffs to an average elevation of about 3,600 feet (1,100 m), approximately 2,400 feet (730 m) above lake level. The base of the Muddy Creek lies at at an unkown depth below this part of Lake Mead. cut into the Grand Wash Cliffs, including an older tributary canyon that the present Colorado river occupies seen on the right and higher up on the walls of the Grand Wash Cliffs behind us.