Moenkopi Formation

The Moenkopi Formation is a geological formation that is spread across the U.S. states of New Mexico, northern Arizona, Nevada, southeastern California, eastern Utah and western Colorado. This unit is considered to be a group in Arizona. Part of the Colorado Plateau and Basin and Range, this red sandstone was laid down in the Lower Triassic[1] and possibly part of the Middle Triassic, around 240 million years ago.[2]

Moenkopi Formation
Stratigraphic range: Lower-Middle Triassic
Moenkopi Formation.jpeg
Rock layers of the Moenkopi Formation in Zion National Park
TypeGeological formation
Sub-unitsSee "Members" section
UnderliesChinle Formation
OverliesKaibab Limestone
Lithology
PrimarySandstone
Location
RegionNorthern Arizona
Southeast California
East-central Nevada
Southern Utah
Northwestern New Mexico
Southwestern Colorado
CountrySouthwestern United States
Type section
Named byWard
Year defined1901

History of investigationEdit

 
Moenkopi Wash in Coconino County, Arizona (1914).

There is no designated type locality for this formation. It was named for a development at the mouth of Moencopie Wash in the Grand Canyon area by Ward in 1901.[3] In 1917 a 'substitute' type locality was located by Gregory in the wall of the Little Colorado Canyon, about 5 miles below Tanner Crossing in Coconino County, Arizona.[citation needed] While in the Great Basin, Bassler and Reeside characterized and named the Rock Canyon Conglomerate, Virgin Limestone, and Shnabkaib Shale members in 1921.[4] Salt Creek (later replaced by Wupatki and Moqui Members) and the Holbrook Member were found and named in the Black Mesa basin by Hager in 1922.[citation needed]

The Sinbad Limestone Member was named in the Paradox Basin by Gilluly and Reeside in 1928. Gregory named the Timpoweap Member in the Plateau sedimentary province in 1948.[citation needed]

The Wupatki Member was first used in the Plateau sedimentary province and its age was modified to Early and Middle(?) Triassic by McKee in 1951.[5] Contacts were revised by Robeck in 1956 and Cooley in 1958. The Tenderfoot, Ali Baba, Sewemup, and Pariott Members were named in the Piceance and Uinta Basins by Shoemaker and Newman in 1959.[6] The Hoskinnini Member was assigned in the Black Mesa and Paradox basins by Stewart in 1959.[7] Contacts were revised again by Schell and Yochelson in 1966. Blakey named the Black Dragon, Torrey, and Moody Canyon members in the Paradox Basin and Plateau sedimentary province in 1974.[8] Contacts were revised yet again by Welsh and others in 1979.

Kietzke modified the age to Early and Middle Triassic using biostratigraphic dating in 1988. The Anton Chico Member was assigned in the Palo Duro Basin and areal limits set by Lucas and Hunt in 1989.[9] In 1991 areal limits were set again by Lucas and Hayden. An overview was completed by Lucas in 1991, Sprinkel in 1994, Hintze and Axen in 1995 and later, Huntoon and others.[10]

DescriptionEdit

The Moenkopi consists of thinly bedded sandstone, mudstone, and shale, with some limestone in the Capitol Reef area. It has a characteristic deep red color and tends to form slopes and benches. The depositional environment varies from fluvial channel and flooplain deposits in the eastern exposures to tidal mudflats in the Cedar Mesa area to deltaic sandstones and shallow marine limestones at Capitol Reef. In eastern Nevada and northwestern Utah, it thickens dramatically, then transitions to the Woodside, Thaynes, and Mahogony formations.[11]

The general deposition setting was sluggish rivers traversing a flat, featureless coastal plane to the sea. The low relief meant that the shoreline moved great distances with changes of sea level or even with the tides. Thickness varies from a feather edge against the Uncompahgre highlands to the east to over 2,000 feet (610 meters) in southwestern Utah. The thickness varies greatly in the Paradox Basin, where the Moenkopi is thin to nonexistent on the crests of salt anticlines and over 400 meters (1,300 feet) thick in the corresponding synclines.[11][2]

The Moenkopi rests unconformably on Paleozoic beds and the Chinle Formation in turn rests unconformably on the Moenkopi. Both unconformities are locally angular unconformities.[12] The lower unconformity corresponds to the regional Tr-1 unconformity and the upper to the regional Tr-3 unconformity. The Tr-1 unconformity represents a hiatus of at least 20 million years while Tr-2 represents a hiatus of about 10 million years.[13]

MembersEdit

Members differ considerably from east to west, in part because sandstone beds corresponding to marine transgressions are used to define members to the west but cannot be traced to the east.[14] In different regions, by ascending stratigraphic order, the members are:

Paradox Basin:[15][16]

  • Tenderfoot Member. This is everywhere in contact with the Cutler Formation on an angular unconformity. Up to 290 feet (88 meters) thick, it consists of basal conglomerate, gypsum, massive cliff-forming mudstone and silty sandstone.
  • Ali Baba Member. This is red conglomeratic sandstone and red siltstone and was laid down by energetic rivers. A distinctive feature is load structures. Sediment sources were apparently the crests of anticlines, and paleocurrent directions are north to northwest, along the corresponding synclines.
  • Sewemup Member. This is thinly bedded siltstone, shale, and sandstone, with enough gypsum content to give it a light brown color that contrasts with the darker brown Ali Baba Member.
  • Parriott Member. This is distinguished from the light brown Sewemup Member by its multihued brown, red, orange and purple strata. Exposures are geographically limited, appearing only in Richardson Amphitheater, Castle Valley, Sinbad Valley, and Big Bend meander of the Colorado River. This member may be separated from the Sewemup Member by a regional unconformity.

Canyonlands and Glen Canyon area:[15]

  • Hoskinnini Member: Sandstone and siltstone. Found only in the southern part of the area.
  • Black Dragon Member. Consists of a basal conglomerate; thinly bedded red sandstone, siltstone, and shale deposited in a tidal flat environment; a sandstone sheet; and a second sequence of tidal flat deposits.
  • Sinbad Limestone Member. Named for the Sinbad region in the San Rafael Swell. Consists of yellowish limestone deposited by a brief marine transgression.
  • Torrey Member. Red beds signifying a return to subaerial deposition.
  • Moody Canyon Member. Thinly bedded slope forming siltstone and mudstone with minor evaporites.

San Juan Basin and Tucumcari:[9]

  • Anton Chico Member. Described previously as the red sandstone member of the Santa Rosa Formation, but placed in its own formation after it was recognized to be middle Triassic in age. Subsequently named as a member of the Moenkopi when its beds were traced west and demonstrated that it was deposited in a single basin with Moenkopi beds in Arizona.

Other members listed in alphabetical order, with asterisks (*) indicating usage by the U.S. Geological Survey and other usages by state geological surveys:[17]

  • Holbrook Sandstone Member (AZ*)
  • Moqui Member (AZ*)
  • Rock Canyon Conglomerate Member (AZ*, NV*, UT*)
  • Shnabkaib Member (AZ*, NV*, UT*)
  • Timpoweap Member (AZ, NV, UT*)
  • Virgin Limestone Member (AZ*, NV*, UT*)
  • Winslow Member (AZ)
  • Wupatki Member (AZ*)

Places visibleEdit

 
The Jurassic through Permian stratigraphy of the Colorado Plateau area of southeastern Utah that makes up much of the famous prominent rock formations in protected areas such as Capitol Reef National Park and Canyonlands National Park. From top to bottom, (Jurassic to Permian):
(6)-Rounded tan domes of the Navajo Sandstone, (5)-(dark)-layered red Kayenta Formation, (4)-cliff-forming, vertically-jointed, red Wingate Sandstone, (3)-slope-forming, purplish Chinle Formation, (2)-layered, lighter-red Moenkopi Formation, and (1)-white, layered Cutler Formation sandstone. Picture from Glen Canyon National Recreation Area, Utah.

Found in these geologic locations:[17]

Found within these parks (incomplete list):

FaunaEdit

 
Eocyclotosaurus .

A diverse fossil vertebrate fauna has been described from the Moenkopi Formation, mainly from the Wupatki Member and Holbrook Member of northern Arizona. Described basal vertebrates include freshwater hybodont sharks, coelacanths, and lungfish. Temnospondyl amphibians are a common component of the fauna. Temnospondyli include Eocyclotosaurus, Quasicyclotosaurus, Wellesaurus, Vigilius, and Cosgriffius. The rhynchosaur Ammorhynchus is known, but rare. Anisodontosaurus is an enigmatic reptile only known from a few tooth-bearing jaws. The poposauroid archosaur Arizonasaurus is known from one relatively complete skeleton and a significant amount of other isolated material. Footprints and several fragmentary body fossils are known from dicynodonts. The footprints of Cheirotherium and Rhynchosauroides are common in the Wupatki Member.

See alsoEdit

FootnotesEdit

  1. ^ Fillmore 2011, p.144
  2. ^ a b c Lucas 2017
  3. ^ Ward 1901
  4. ^ Bassler and Reeside 1921
  5. ^ McKee 1951
  6. ^ Shoemaker and Newman 1959
  7. ^ Stewart 1959
  8. ^ Blakey 1974
  9. ^ a b Lucas and Hunt 1989
  10. ^ For the whole section, except where noted: GEOLEX database Bibliographic References
  11. ^ a b Fillmore 2011, p.143
  12. ^ Lucas 2017, p.149
  13. ^ Lucas 2017, p.155
  14. ^ Fillmore 2011, p.142
  15. ^ a b Fillmore 2011, p.148-154
  16. ^ Lucas 2017, p. 151
  17. ^ a b GEOLEX database: Moenkopi

ReferencesEdit

  • Bassler, Harvey; Reeside, J.B., Jr. (1921), "Oil prospects in Washington County, Utah" (PDF), Contributions to economic geology, 1921; Part 2, Mineral fuels, U.S. Geological Survey Bulletin, 726-C, pp. C87–C107, retrieved 26 May 2020
  • Blakey, R.C. (1974). "Stratigraphic and depositional analysis of the Moenkopi Formation, southeastern Utah". Utah Geological and Mineral Survey Bulletin. 104.
  • Fillmore, Robert (2011). Geological evolution of the Colorado Plateau of eastern Utah and western Colorado, including the San Juan River, Natural Bridges, Canyonlands, Arches, and the Book Cliffs. University of Utah Press. ISBN 978-1-60781-004-9.
  • Lucas, Spencer G. (2017). "Triassic-Jurassic stratigraphy in southwestern Colorado" (PDF). New Mexico Geological Society Field Conference Series. 68: 149–158. Retrieved 26 May 2020.
  • Lucas, S.G.; Hunt, A.P. (1989). "Revised Triassic stratigraphy in the Tucumcari basin, east-central New Mexico". In Lucas, S.G.; Hunt, A.P. (eds.). Dawn of the age of dinosaurs in the American southwest. New Mexico Museum of Natural History and Science. pp. 150–170.
  • McKee, E.D. (1951). "Triassic deposits of the Arizona-New Mexico border area" (PDF). New Mexico Geological Society Field Conference Series. 2, : 85. Retrieved 26 May 2020.CS1 maint: extra punctuation (link)
  • Shoemaker, Eugene M.; Newman, William L. (1959). "Moenkopi Formation (Triassic? and Triassic) in Salt Anticline Region, Colorado and Utah". AAPG Bulletin. 43. doi:10.1306/0BDA5E70-16BD-11D7-8645000102C1865D.
  • John H. Stewart (2) (1959). "Stratigraphic Relations of Hoskinnini Member (Triassic?) of Moenkopi Formation on Colorado Plateau". AAPG Bulletin. 43. doi:10.1306/0BDA5E73-16BD-11D7-8645000102C1865D.
  • Ward, Lester F. (Dec 1901). "Geology of the Little Colorado Valley". American Journal of Science. New Haven. 12 (72): 401.
  • GEOLEX database entry for Moenkopi, USGS [Accessed 18 March 2006] (public domain text)
  • Bibliographic References for Moenkopi [Accessed 18 March 2006]