Jump to content

Wingate Sandstone

Coordinates: 39°06′N 109°06′W / 39.1°N 109.1°W / 39.1; -109.1
From Wikipedia, the free encyclopedia
(Redirected from Wingate Formation)
Wingate Sandstone
Stratigraphic range: Rhaetian-Hettangian
~206–199 Ma
Wingate Sandstone cliffs in the San Rafael Swell, Utah
TypeGeological formation
Unit ofGlen Canyon Group
UnderliesKayenta Formation
OverliesChinle Formation
Lithology
PrimaryEolian sandstone
Location
Coordinates39°06′N 109°06′W / 39.1°N 109.1°W / 39.1; -109.1
Approximate paleocoordinates17°42′N 48°18′W / 17.7°N 48.3°W / 17.7; -48.3
Regionnorthern Arizona, northwest Colorado, Nevada, Utah
Country United States
ExtentColorado Plateau
Type section
Named forFort Wingate
Named byC.E. Dutton
Wingate Sandstone is located in the United States
Wingate Sandstone
Wingate Sandstone (the United States)
Wingate Sandstone is located in Utah
Wingate Sandstone
Wingate Sandstone (Utah)

The Wingate Sandstone is a geologic formation in the Glen Canyon Group of the Colorado Plateau province of the United States which crops out in northern Arizona, northwest Colorado, Nevada, and Utah.

Geology

[edit]

Wingate Sandstone is particularly prominent in southeastern Utah, where it forms attractions in a number of national parks and monuments. These include Capitol Reef National Park, the San Rafael Swell, and Canyonlands National Park.

Wingate Sandstone frequently appears just below the Kayenta Formation and Navajo Sandstone, two other formations of the Glen Canyon group. Together, these three formations can result in immense vertical cliffs of 2,000 feet (610 meters) or more. Wingate layers are typically pale orange to red in color, the remnants of wind-born sand dunes deposited approximately 200 million years ago in the Late Triassic.

Fossil content

[edit]

Long dated to the Early Jurassic only, fossils (including a phytosaur skull) and other evidence indicate that part of the Wingate Sandstone is as old as Late Triassic in age. The upper part of the formation, which laterally interfingers with the Moenave Formation to the west, is Early Jurassic in age.[1][2]

[edit]

References

[edit]
  1. ^ Lucas, S. G., A. B. Heckert, J. W. Estep, and O. J. Anderson. 1997. Stratigraphy, biostratigraphy, and sequence stratigraphy of the Upper Triassic Chinle Group, Four Corners region. Pages 81-107 in Anderson, O. J., B. Kues, and S. G. Lucas, editors. Mesozoic geology and paleontology of the Four Corners Region. New Mexico Geological Society, Socorro, NM. New Mexico Geological Society, 48th Field Conference.
  2. ^ Lucas, S. G., A. B. Heckert, and L. H. Tanner. 2005. Arizona’s Jurassic fossil vertebrates and the age of the Glen Canyon Group. Pages 95-104 in Heckert, A. B. and S. G. Lucas (editors). Vertebrate paleontology in Arizona. New Mexico Museum of Natural History and Science, Albuquerque, NM. Bulletin 29.
[edit]