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  2. Sixtymile Formation - Wikipedia

    en.wikipedia.org/wiki/Sixtymile_Formation

    Blakey, Ron and Wayne Ranney, Ancient Landscapes of the Colorado Plateau, Grand Canyon Association (publisher), 2008, 176 pages, ISBN 978-1934656037 Chronic, Halka. Roadside Geology of Arizona, Mountain Press Publishing Co., 1983, 23rd printing, pp. 229–232, ISBN 978-0878421473

  3. Geology of the Grand Canyon area - Wikipedia

    en.wikipedia.org/wiki/Geology_of_the_Grand...

    Grand Canyon lies on the southern end of the Intermountain West seismic belt. [84] At least 35 earthquakes larger than 3.0 on the Richter Scale occurred in the Grand Canyon region in the 20th century. [85] Of these, five registered over 5.0 on the Richter Scale and the largest was a 6.2 quake that occurred in January 1906. [85]

  4. Hermit Formation - Wikipedia

    en.wikipedia.org/wiki/Hermit_Formation

    As summarized by McKee in 1982, [3] the sedimentary strata assigned to the Supai Group and Hermit Formation have a long and complicated nomenclature. However, out of numerous publications, three major papers have been responsible for the defining the Hermit Formation as currently mapped in the Grand Canyon region [1] First in 1910, Darton [4] proposed the name of Supai Formation for ...

  5. Toroweap Overlook - Wikipedia

    en.wikipedia.org/wiki/Toroweap_Overlook

    Toroweap Overlook (also known as Tuweep Overlook or Toroweap Point) is a viewpoint within the Grand Canyon National Park in Arizona, United States. It is located in a remote area on the North Rim of the Grand Canyon , 55 miles (89 km) west of the North Rim Headquarters (but 148 miles (238 km) by road).

  6. Tonto Group - Wikipedia

    en.wikipedia.org/wiki/Tonto_Group

    Figure 1. A geologic cross section of the Grand Canyon. [5]The Tonto Group is a name for an assemblage of related sedimentary strata, collectively known by geologists as a Group, that comprises the basal sequence Paleozoic strata exposed in the sides of the Grand Canyon.

  7. Muav Limestone - Wikipedia

    en.wikipedia.org/wiki/Muav_Limestone

    The Muav Limestone forms cliffs or small ledges that weather a dark gray or rusty-orange color. These cliffs or small ledges directly overlie the sloping surfaces of the Bright Angel Shale. The thickness of this formation decreases eastward from 76 m (249 ft) in the western Grand Canyon to 14 m (46 ft) in the eastern Grand Canyon.

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