Cutler Formation

The Cutler Formation or Cutler Group is a rock unit that is spread across the U.S. states of Arizona, northwest New Mexico, southeast Utah and southwest Colorado. It was laid down in the Early Permian during the Wolfcampian stage. Its subunits, therefore, are variously called formations or members depending on the publication. Members (youngest to oldest):[1][2]

Cutler Formation
Stratigraphic range:
Early Permian
Cedar Mesa Sandstone overlaying Organ Rock Shale, Canyonlands, Utah
TypeGeological formation
Sub-unitsDe Chelly Sandstone,
White Rim Sandstone,
Organ Rock Shale,
Cedar Mesa Sandstone,
Elephant Canyon Formation,
Halgaito Shale[1][2]
UnderliesChinle Formation
Lithology
PrimaryIron-rich arkose sandstone
Location
Coordinates38.096°N 107.702°W / 38.096; -107.702
Approximate paleocoordinates0.7°N 36.1°W / 0.7; -36.1
RegionColorado Plateau
Country United States
Extent Arizona
 Colorado
 New Mexico
 Utah
Type section
Named forCutler Creek, north of Ouray, Co
Named byCross & Howe
Year defined1905
Cutler Formation (the United States)
Cutler Formation (New Mexico)
The Permian through Jurassic 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: Rounded tan domes of the Navajo Sandstone, layered red Kayenta Formation, cliff-forming, vertically-jointed, red Wingate Sandstone, slope-forming, purplish Chinle Formation, layered, lighter-red Moenkopi Formation, and white, layered Cutler Formation sandstone. Picture from Glen Canyon National Recreation Area, Utah.

Extent

There is no designated type locality for the Cutler. It was named by Cross and Howe in 1905 after Cutler Creek, which enters Uncompahgre River about 4 miles north of Ouray, Colorado.[3] Baker and Reeside revised Cross and Howe's work in 1929 by dividing the formation into the Halgaito Tongue (base), Cedar Mesa Sandstone Member, Organ Rock Tongue, and White Rim Sandstone Member. Cutler's geographic extent was established by Wood and Northrop in 1946. In 1958 Wengerd and Matheny raised the formation to group rank.

Geology

Cutler outcrops are found in these geologic locations in Arizona, Colorado, New Mexico and Utah.

References
  1. "Geology of Canyonlands National Park" (PDF). National Park Service, U.S. Department of the Interior. Retrieved 30 September 2018.
  2. "Stratigraphy of Canyon de Chelly National Monument". Geology of National Parks, 3D and Photographic Tours. United States Geological Survey. Archived from the original on 1 October 2018. Retrieved 30 September 2018.
  3. Keroher, Grace C., Lexicon of Geologic Names of the United States for 1936-1960, Part 1, p. 1019, at Google Books

Bibliography
  • Cross, C.W. and Howe, Ernest, 1905, "Geography and general geology of the quadrangle, IN Description of the Silverton quadrangle [Colorado]", U.S. Geological Survey Geologic Atlas of the United States, Silverton folio, no. 120, 34 p.
  • Baker, A.A. and Reeside, J.B., Jr., 1929, "Correlation of the Permian of southern Utah, northern Arizona, northwestern New Mexico, and southwestern Colorado", American Association of Petroleum Geologists Bulletin, v. 13, no. 11, p. 1413-1448
  • Wood, G.H. and Northrop, S.A., 1946, "Geology of Nacimiento Mountains, San Pedro Mountain, and adjacent plateaus in parts of Sandoval and Rio Arriba Counties, New Mexico", U.S. Geological Survey Oil and Gas Investigations Map, OM-57, 1 sheet, scale 1:95,040
  • Wengerd, S.A. and Matheny, M.L., 1958, "Pennsylvanian system of the Four Corners region", American Association of Petroleum Geologists Bulletin, v. 42, no. 9, p. 2048-2106
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