Muav Limestone

Muav Limestone
Stratigraphic range: Middle Cambrian[1][2]

representative sequence of Redwall, Temple Butte, and Muav Limestone, in Grand Canyon
Type Geological formation
Unit of Tonto Group
Underlies Redwall Limestone (Mississippian). Locally underlies Temple Butte Limestone (Devonian) that fills narrow paleovalleys cut into the unconformity separating the Redwall Limestone from Muav Limestone.
Overlies Bright Angel Shale
Thickness 650 feet (200 m), at maximum
Lithology
Primary limestone and dolomite
Other calcareous mudstone
Location
Region Northern Arizona (Grand Canyon), central Arizona, southeast California, southern Nevada, and southeast Utah
Country United States of America
Type section
Named for Muav Canyon, north side of Colorado River[3]
Named by Noble (1914)[3]

The Cambrian Muav Limestone is the upper geologic unit of the 3-member Tonto Group. It is about 650 feet (198 m) thick at its maximum.[4] It is a resistant cliff-forming unit. The Muav consists of dark to light-gray, brown, and orange red limestone with dolomite and calcareous mudstone.[5] The Muav is overlain in some areas by the Devonian Temple Butte Limestone, but the major unit above are the vertical cliffs of Mississippian Redwall Limestone. The Muav is located in the lower elevations of the Grand Canyon, Arizona.[6]

The Muav is in-part younger than, and in-part grades into, the Bright Angel Shale which is less erosion resistant and is categorized as a slope-forming unit. The Muav is about 350 feet thick in the east and reaches about 600 feet thick in the western part of its exposure area in the Grand Canyon.[5] The two units lie above the erosion-resistant cliff-forming Tapeats Sandstone. In the eastern canyon, the Tapeats creates the horizontal Tonto Platform. In west Grand Canyon, the north-south Toroweap Fault is the west perimeter of the Tonto Platform, and west Grand Canyon is dominated by the erosion resistant unit of the Esplanade Sandstone. The Tonto Trail is a mostly horizontal trail on the south side of Granite Gorge, on the platform.

The Tonto Group units were deposited on an ancient erosion surface (angular unconformity) on the Vishnu Basement Rocks. The Vishnu sequence has a dip of about 45 degrees. As this unconformity represents about 1,000 million years (1.0 billion years) of non–deposition, tectonic activity and erosion on the Vishnu Basement Rocks is called the Great Unconformity.

Beyond the Grand Canyon area the Muav occurs in southern Utah, southern Nevada and southern California. In the California occurrence it is known as the Muav Marble.[5]

Geologic sequence

The units of the Tonto Group:

See also

References

  1. ↑ Rose, E. (2006) "Nonmarine aspects of the Cambrian Tonto Group of the Grand Canyon, USA, and broader implications". Palaeoworld. 15:223–241.
  2. ↑ Rose, E (2011) Modification of the nomenclature and a revised deposition model for the Cambrian Tonto Group of the Grand Canyon, Arizona. in JS Hollingsworth, FA Sundberg, and JR Foster, eds., pp 77-98, Cambrian Stratigraphy and Paleontology of Northern Arizona and Southern Nevada: Museum of Northern Arizona Bulletin 67, 321 p.
  3. 1 2 Noble, LF (1914) The Shinumo quadrangle, Grand Canyon district, Arizona. Bulletin no. 549, US Geological Survey, Reston, Virginia.
  4. ↑ Chronic, H (1983) Roadside Geology of Arizona. The Mountaineers Books, Seattle, Washington. (softcover, ISBN 978-0-87842-147-3) p. 179.
  5. 1 2 3 Anonymous (2006d) Muav Limestone, Stratigraphy of the Parks of the Colorado Plateau. U.S. Geological Survey, Reston, Virginia.
  6. ↑ Hampton, HM (1998) Geologic Map of the Grand Canyon in the Vicinity of the South Rim Visitor Center. in Kamilli, RJ, and SM Richard, eds., Geologic Highway Map of Arizona, Arizona Geological Society and Arizona Geological Survey, 1 sheet, scale 1:62,500.

Gallery--Muav Limestone

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