Cedar Mesa Sandstone
Stratigraphic range: Early Permian-Early Triassic,
Cedar Mesa Formation at its type location, capping Cedar Mesa, Utah
TypeGeological member[1]
Unit ofCutler Formation
UnderliesOrgan Rock Shale
OverliesElephant Canyon Formation
Halgaito Member
ThicknessOver 1,000 feet (300 m)
Lithology
PrimarySandstone
Location
Coordinates37°23′N 109°55′W / 37.383°N 109.917°W / 37.383; -109.917
RegionColorado Plateau
CountryUnited States
Type section
Named forCedar Mesa
Named byArthur A. Baker
John B. Reeside, Jr., 1929
Cedar Mesa Sandstone is located in the United States
Cedar Mesa Sandstone
Cedar Mesa Sandstone (the United States)
Cedar Mesa Sandstone is located in Utah
Cedar Mesa Sandstone
Cedar Mesa Sandstone (Utah)
Druid Arch in Canyonlands National Park, an eroded fin of Cedar Mesa Sandstone

Cedar Mesa Sandstone (also known as the Cedar Mesa Formation) is a sandstone member[1] of the Cutler Formation, found in southeast Utah, southwest Colorado, northwest New Mexico, and northeast Arizona.[2]

Description

The Cedar Mesa Sandstone consists mainly of red and white sandstone showing cross-bedding typical of an eolian sandstone.[3] The thick beds of cross-bedded sandstone are separated by thin layers of siltstone or other softer rock that erodes more easily, forming horizontal recesses.[4] These have been traced for over 200 kilometers (120 mi) and contain rhizoliths (fossil roots) and other indications that a thin soil layer developed.[5] At its type location at Cedar Mesa near the San Juan River in Utah, the sandstone is 500 feet (150 m) to over 1,000 feet (300 m) thick. Drill holes near Glen Canyon have penetrated more than 1,200 feet (370 m) of Ceder Mesa beds.[6] To the southeast, at the limits of surface exposure, the sandstone intertongues with beds of gypsum, siltstone, and limestone, which continue into the subsurface for another 125 kilometers (78 mi).[7] The sandstone is assigned to the Cutler Formation, and overlies the Halgaito Member and in turn is overlain by the Organ Rock Member.[8] North and northeast of the confluence of the Colorado and Green Rivers, the sandstone intertongues with undifferentiated Cutler Formation beds.[9]

The Cutler is raised to group rank in some areas of the Colorado Plateau, and its members, including the Cedar Mesa Sandstone, are then raised to formation rank.[10]

In addition to capping Cedar Mesa,[8][2] the Cedar Mesa Sandstone forms the spires and canyons found in the Needles and Maze districts of Canyonlands National Park,[11] the inner gorge of White Canyon,[12] and the three natural bridges of Natural Bridges National Monument.[13][9] The sandstone continues in the subsurface into the Four Corners region.[9]

Cedar Mesa Sandstone is the remains of coastal sand dunes deposited about 270 to 300 million years ago, during the Wolfcampian (early Permian).[14] The red and white banded appearance is a result of periodic floods which carried iron-rich sediments down from the Uncompahgre Mountains during its formation.[15][11][16][6] The cross-bedding dips consistently to the southeast, showing that prevailing winds were from the northwest, and the source of the sand making up the sandstone was the shallow sea to the west and north.[4]

The origin of the thin layers of softer rock is not settled,[5] but one possibility is that these layers developed at times when the water table rose. This cut off the supply of sand, and wind erosion then eroded the dune field flat at the level of the water table, where a thin soil developed and became vegetated.[17]

The interbedded gypsum, siltstone, and limestone to the southeast are interpreted as sabkha deposits, deposited in saline coastal flats.[7]

Fossils

Fragmented fossils are found in some of the thin layers of softer rock. These include large (up to 1 by 8 meters (3 ft 3 in by 26 ft 3 in)) petrified conifer logs, small horsetail (Equisetum) stem fragments, and fern leaves resembling Asterotheca. These are thought to have been brought into the dune field by large flood events. Reptile bones and teeth, including a possible jaw fragment of a pelycosaur, have also been found in the formation.[5]

History of investigation

The beds belonging to the unit were originally assigned to the Coconino Sandstone of northern Arizona, but were reassigned to the Cedar Mesa sandstone member of the Cutler Formation by A.A. Baker and John B. Reeside, Jr., in 1929. They named the member for its exposures capping Cedar Mesa.[8] S.A. Wengerd and M.L. Matheny recommended raising the Cedar Mesa Sandstone to formation rank in 1958.[10]

See also

References

  1. 1 2 The Cutler Formation is sometimes classified as the Cutler Group, in which case Cedar Mesa Sandstone is classified as a formation rather than a member.
  2. 1 2 "Cedar Mesa Sandstone". Park Stratigraphy of the Colorado Plateau. United States Geological Survey. Archived from the original on 23 June 2010. Retrieved 25 November 2009.
  3. ↑ Fillmore, Robert (2010). 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. Salt Lake City: University of Utah Press. pp. 120–126. ISBN 9781607810049.
  4. 1 2 Fillmore 2010, p. 124.
  5. 1 2 3 Stanesco, J.D.; Campbell, J.A. (1989). "Eolian and Noneolian Facies of the Lower Permian Cedar Mesa Sandstone Member of the Cutler Formation, Southeastern Utah". U.S. Geological Survey Bulletin. 1808-F: F1. doi:10.3133/b1808EF.
  6. 1 2 Fillmore 2010, p. 121.
  7. 1 2 Stanesco & Campbell 1989, pp. F9–F10.
  8. 1 2 3 Baker, A.A.; Reeside, J.B. Jr. (1929). "Correlation of the Permian of Southern Utah, Northern Arizona, Northwestern New Mexico, and Southwestern Colorado". AAPG Bulletin. 13 (11): 1413–1448. doi:10.1306/3D932893-16B1-11D7-8645000102C1865D.
  9. 1 2 3 Fillmore 2010, p. 120.
  10. 1 2 Wengerd, S.A.; Matheny, M.L. (1958). "Pennsylvanian System of Four Corners Region". AAPG Bulletin. 42 (9): 2048–2106. doi:10.1306/0BDA5BA9-16BD-11D7-8645000102C1865D.
  11. 1 2 "Canyonlands National Park - Cedar Mesa Sandstone". National Park Service. Retrieved 25 November 2009.
  12. ↑ "Geological Survey Circular 217 - Preliminary Report on the White Canyon Area, San Juan County, Utah". United States Geological Survey. Retrieved 25 November 2009.
  13. ↑ "Natural Bridges - Geology" (PDF). National Park Service. January 2003. Retrieved 25 November 2009.
  14. ↑ Baars, D.L. (1962). "Permian System of Colorado Plateau". AAPG Bulletin. 46 (2): 149–218. doi:10.1306/BC74376F-16BE-11D7-8645000102C1865D.
  15. ↑ Langford, Richard; Chan, Marjorie A. (1 October 1988). "Flood surfaces and deflation surfaces within the Cutler Formation and Cedar Mesa Sandstone (Permian), southeastern Utah". GSA Bulletin. 100 (10): 1541–1549. doi:10.1130/0016-7606(1988)100<1541:FSADSW>2.3.CO;2.
  16. ↑ "Canyonlands National Park - Geologic Formations". National Park Service. Retrieved 26 November 2009.
  17. ↑ Fillmore 2010, pp. 124–125.


This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.