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Cambrian The Cambrian Period ( ; sometimes symbolized Ꞓ) was the first geological period of the Paleozoic Era, and of the Phanerozoic Eon. The Cambrian lasted 53.4 million years from the end of the preceding Ediacaran Period 538.8 million years ag ...
Muav Limestone is a
geologic unit A stratigraphic unit is a volume of rock of identifiable origin and relative age range that is defined by the distinctive and dominant, easily mapped and recognizable petrographic, lithologic or paleontologic features (facies) that characterize ...
within the 5-member
Tonto Group 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. As currently defined, the T ...
. It is about thick at its maximum. It is a resistant cliff-forming unit. The Muav consists of dark to light-gray, brown, and orange red
limestone Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms wh ...
with dolomite and calcareous mudstone.Karlstrom, K.E., Mohr, M.T., Schmitz, M.D., Sundberg, F.A., Rowland, S.M., Blakey, R., Foster, J.R., Crossey, L.J., Dehler, C.M. and Hagadorn, J.W., 2020. ''Redefining the Tonto Group of Grand Canyon and recalibrating the Cambrian time scale''. ''Geology'', 48(5), pp. 425–430.Connors, T.B., Tweet, J.S., and Santucci, V.L., 2020. ''Stratigraphy of Grand Canyon National Park''. In: Santucci, V.L., Tweet, J.S., ed., pp. 54–74, ''Grand Canyon National Park: Centennial Paleontological Resource Inventory (Non-sensitive Version) ''. Natural Resource Report NPS/GRCA/NRR—2020/2103. National Park Service, Fort Collins, Colorado, 603 pp. The Muav Limestone is overlain in the western Grand Canyon by the late
Cambrian The Cambrian Period ( ; sometimes symbolized Ꞓ) was the first geological period of the Paleozoic Era, and of the Phanerozoic Eon. The Cambrian lasted 53.4 million years from the end of the preceding Ediacaran Period 538.8 million years ag ...
Frenchman Mountain Dolostone. Eastward, the Frenchman Mountain Dolostone pinches out and the
Mississippian Mississippian may refer to: * Mississippian (geology), a subperiod of the Carboniferous period in the geologic timescale, roughly 360 to 325 million years ago *Mississippian culture, a culture of Native American mound-builders from 900 to 1500 AD ...
Redwall Limestone, which forms prominent vertical cliffs, directly lies upon the Muav Limestone. The
Devonian The Devonian ( ) is a geologic period and system of the Paleozoic era, spanning 60.3 million years from the end of the Silurian, million years ago (Mya), to the beginning of the Carboniferous, Mya. It is named after Devon, England, w ...
Temple Butte Formation The Devonian Temple Butte Formation, also called Temple Butte Limestone, outcrops through most of the Grand Canyon of Arizona, USA; it also occurs in southeast Nevada. Within the eastern Grand Canyon, it consists of thin, discontinuous and rela ...
fill deep paleovalleys that have been cut through the Frenchman Mountain Dolostone and into the Muav Limestone. The Muav is in part younger than, and in-part grades into, the
Bright Angel Shale The Cambrian Bright Angel Shale is the middle layer of the three member Tonto Group geologic feature. The 3-rock Tonto section famously sits upon the Great Unconformity because of the highly resistant cliffs of the base layer, vertical Tapeats S ...
, 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.Anonymous (2006d
''Muav Limestone''


. U.S. Geological Survey, Reston, Virginia.
The two units lie above the erosion-resistant cliff-forming Tapeats Sandstone. In the eastern canyon, the Tapeats Sandstone creates the extremely 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 The Tonto Trail is a hiking trail on the South Rim of the Grand Canyon in Grand Canyon National Park, located in the U.S. state of Arizona. Access The Tonto Trail does not terminate at either rim of the Grand Canyon, but begins along the south b ...
is a mostly horizontal trail on the south side of Granite Gorge, on the Tonto Platform. The Tonto Group units were deposited on an ancient
erosion surface In geology and geomorphology, an erosion surface is a surface of rock or regolith that was formed by erosion and not by construction (e.g. lava flows, sediment deposition) nor fault displacement. Erosional surfaces within the stratigraphic ...
(
angular unconformity An unconformity is a buried erosional or non-depositional surface separating two rock masses or strata of different ages, indicating that sediment deposition was not continuous. In general, the older layer was exposed to erosion for an interval o ...
) on the Vishnu Basement Rocks. The Vishnu sequence has a dip of about 45 degrees. As this long-timeframe unconformity represents about 1,000 million years (1.0 billion years) of non–deposition, tectonic activity and erosion, on the
Vishnu Basement Rocks The Vishnu Basement Rocks is the name recommended for all Early Proterozoic crystalline rocks (metamorphic and igneous) exposed in the Grand Canyon region. They form the crystalline basement rocks that underlie the Bass Limestone of the Unkar ...
, is called the
Great Unconformity Of the many unconformities (gaps) observed in geological strata, the term Great Unconformity is frequently applied to either the unconformity observed by James Hutton in 1787 at Siccar Point in Scotland,Rance, H (1999''Historical Geology: The ...
. Beyond the Grand Canyon area the Muav occurs in southern
Utah Utah ( , ) is a state in the Mountain West subregion of the Western United States. Utah is a landlocked U.S. state bordered to its east by Colorado, to its northeast by Wyoming, to its north by Idaho, to its south by Arizona, and to its ...
, southern
Nevada Nevada ( ; ) is a state in the Western region of the United States. It is bordered by Oregon to the northwest, Idaho to the northeast, California to the west, Arizona to the southeast, and Utah to the east. Nevada is the 7th-most extensive, ...
and southern
California California is a state in the Western United States, located along the Pacific Coast. With nearly 39.2million residents across a total area of approximately , it is the most populous U.S. state and the 3rd largest by area. It is also the ...
. In the California occurrence it is known as the Muav Marble.


Geologic sequence

The units of the Tonto Group: * 5 – Frenchman Mountain Dolostone * 4 – Muav Limestone * 3 – Bright Angel Shale * 2 – Tapeats Sandstone (start of
transgression Transgression may refer to: Legal, religious and social *Sin, a violation of God's Ten Commandments or other elements of God's moral law *Crime, legal transgression, usually created by a violation of social or economic boundary **In civil law ju ...
series) * 1 – Sixtymile Formation


Gallery – Muav Limestone

File:Grand Canyon National Park, North Kaibab Trail in Redwall 0990 - Flickr - Grand Canyon NPS.jpg, upright=1.2, Muav Limestone cliff example, below Redwall Limestone cliff, on the
North Kaibab Trail The North Kaibab Trail is a hiking trail in the North Rim side of the Grand Canyon, in Grand Canyon National Park, located in the U.S. state of Arizona. Access Access to this part of the park by car is seasonal, open from mid-May to mid-Octo ...
(closeup photos, often show purple erosion debris)(expandable photo) File:Grand Canyon01.jpg, (view due-north, northeast, from
Bright Angel Trail The Bright Angel Trail is a hiking trail located in Grand Canyon National Park in the U.S. state of Arizona. Description The trail originates at Grand Canyon Village on the south rim of the Grand Canyon, descending 4380 feet to the Colorad ...
, (''South Rim section'') – View of south-draining Bright Angel Canyon, containing in its lowest section with the Tapeats Sandstone, upon the Granite Gorge, the ''cliffs of gray-brown'' Muav Limestone (25% at base of Redwall Limestone), laid upon the ''slope-forming & greenish'' Bright Angel Shale. (The trail also descends/ascends through units on the South Rim, at near photo view.) File:Grand Canyon-Mather point.jpg, View to Sumner Butte, Redwall Limestone peak & vertical cliff, sitting on Muav Limestone


See also

*
Geology of the Grand Canyon area The geology of the Grand Canyon area includes one of the most complete and studied sequences of rock on Earth. The nearly 40 major sedimentary rock layers exposed in the Grand Canyon and in the Grand Canyon National Park area range in age from ab ...


References


Further reading

* Blakey, and Ranney, 2008. ''Ancient Landscapes of the Colorado Plateau'', Ron Blakey, Wayne Ranney, c 2008, Grand Canyon Association (publisher), 176 pages, with Appendix, Glossary, Index. Contains approximately 75 shaded topographic maps, for geology, etc., with 54 (23 pairs, (46)) for
Colorado Plateau The Colorado Plateau, also known as the Colorado Plateau Province, is a physiographic and desert region of the Intermontane Plateaus, roughly centered on the Four Corners region of the southwestern United States. This province covers an area ...
specifically; others are global, or North American. * Arizona Geological Society,
Arizona Geological Survey The Arizona Geological Survey (AZGS) was established by the Arizona Legislature to investigate and describe Arizona's geology and to educate and inform the public regarding its geologic setting. Each year since 1915, AZGS has released geologic m ...
, c. 1998 (etc.) ''Geologic Highway Map of Arizona.'' Contains geologic map, Arizona Shaded Relief Map, Geologic Cross Sections, Shaded Relief Map of Arizona, ''Geologic Map of the
Grand Canyon The Grand Canyon (, yuf-x-yav, Wi:kaʼi:la, , Southern Paiute language: Paxa’uipi, ) is a steep-sided canyon carved by the Colorado River in Arizona, United States. The Grand Canyon is long, up to wide and attains a depth of over a ...
in the Vicinity of the South Rim Visitor Center'', etc.


External links

{{commons category, Muav Limestone * Abbot, W, (2001
''Revisiting the Grand Canyon – Through the Eyes of Seismic Sequence Stratigraphy.''Search and Discovery Article # 40018
America Association of Petroleum Geologists, Tulsa, Oklahoma. * Anonymous (2006a

U.S. Geological Survey, Reston, Virginia. * Anonymous (2006b

U.S. Geological Survey, Reston, Virginia. * Anonymous (2006c

U.S. Geological Survey, Reston, Virginia. * Anonymous (2006d

U.S. Geological Survey, Reston, Virginia. * Hartman, J. H. (2001
''Muav Limestone, Grand Canyon National Park, Coconino County, Arizona.''GeoDIL, A Geoscience Digital Image Library
University of North Dakota, Grand Forks, North Dakota. * Mathis, A., and C. Bowman (2007
''The Grand Age of Rocks: The Numeric Ages for Rocks Exposed within Grand Canyon''Grand Canyon National Park, Arizona
National Park Service, Grand Canyon National Park, Arizona. * Noble, L. F. (1923a
Unconformity between Temple Butte limestone and Muav limestone, Coconino County, Arizona, Plate 22-A.
Reston, Virginia. * Noble, L. F. (1923b
Unconformity between Temple Butte limestone and Muav limestone, Coconino County, Arizona, Plate 22-B.
Reston, Virginia. * Noble, L. F. (1923c
Unconformity between Temple Butte limestone and Muav limestone, Coconino County, Arizona, Plate 23-A.
Reston, Virginia. * Rowland, S. (nda
Department of Geoscience
University of Nevada, Las Vegas, Nevada. * Rowland, S. (ndb
Department of Geoscience
University of Nevada, Las Vegas, Nevada. * Stamm, N. (2013
National Geologic Database
U.S. Geological Survey, Reston, Virginia. * Timmons, S. S. (2003

National Park Service, Grand Canyon National Park, Arizona. Limestone formations of the United States Natural history of the Grand Canyon Geologic formations of Arizona Geologic formations of Nevada Cambrian Arizona Cambrian Nevada Cambrian System of North America