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The Kayenta Formation frequently appears as a thinner dark broken layer below Navajo Sandstone and above Wingate Sandstone (all three formations are in the same group). Together, these three formations can result in immense vertical cliffs of 600 metres (2,000 ft) or more. Kayenta layers are typically red to brown in color, forming broken ledges.
The Kayenta Formation pinches out and disappears to the north, in the Uintah Basin, and the Wingate Sandstone and Navajo Sandstone become indistinguishable. These remaining eolian beds have sometimes been mapped as simply Glen Canyon Formation, but they correlate with the Nugget Sandstone further north, and it has been recommended that they be ...
Kayentasuchus (meaning "Kayenta Formation crocodile") is a genus of sphenosuchian, a type of basal crocodylomorph, the clade that comprises the crocodilians and their closest kin. It is known from a single skeleton found in rocks of the Sinemurian-Pliensbachian-age Lower Jurassic Kayenta Formation, northeastern Arizona.
Fossilized footprints of dinosaurs and the crocodile-like tritylodonts can be found in this 350 foot (107 m) thick ledgy-slope forming formation, called the Kayenta. [7] The Kayenta weathers into three units; a lower ledge and middle cliff that are dominated by cross-bedded sandstone and an upper slope that has relatively more siltstone.
The next member in the Moenave Formation is the thin-bedded Whitmore Point, which is made of mudstone and shale. [11] The lower red cliffs visible from the Zion Human History Museum (until 2000 the Zion Canyon Visitor Center) are accessible examples of this formation. [3] Kayenta Formation
Parting lineation, from lower right to upper left; Kayenta Formation, Canyonlands National Park. The Glen Canyon Group of formations includes (from oldest - lowest - to youngest) the Wingate Sandstone, Kayenta Formation, and the; Navajo Sandstone; These formations are most prominently exposed in the western and northern sections of the park.
The Chinle Formation was then laid down on top of this eroded surface. Increasingly dry climates dominated the Triassic. Therefore, sand in the form of sand dunes invaded and became the Wingate Sandstone. For a time climatic conditions became wetter and streams cut channels through the sand dunes, forming the Kayenta Formation.
Kayentatherium means "Kayenta Beast", and is named for the geological formation in which it was found, the Kayenta Formation. Kayentatherium is known from several specimens. [ 1 ] [ 2 ] The specific name honors paleontologist Samuel Welles , who worked with the University of California Museum of Paleontology in much of the pioneering work on ...