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The Kayenta Formation is a geological formation in the Glen Canyon Group that is spread across the Colorado Plateau province of the United States, including northern Arizona, northwest Colorado, Nevada, and Utah. Traditionally has been suggested as Sinemurian -Pliensbachian, but more recent dating of detrital zircons has yielded a depositional ...
The Kayenta Formation is a stratigraphic unit within the Triassic-Jurassic Glen Canyon Group, which crops out across the Colorado Plateau. Despite extensive outcrop of the "typical facies" of the Kayenta Formation in Utah , Colorado , and northern Arizona, vertebrate fossils are rare in these regions.
S. kayentakatae was a relatively small dinosaur, reaching 2.5 m (8.2 ft) in length and 30 kg (66 lb) in body mass. [ 12] It had two small, parallel crests which may demonstrate an evolutionary step toward later and larger neotheropods, such as the more advanced and larger Dilophosaurus. Both possess a "weak joint" between the premaxillary and ...
Welles, 1954. Dilophosaurus (/ daɪˌloʊfəˈsɔːrəs, - foʊ -/ [1] dy-LOH-fə-SOR-əs, -foh-) is a genus of theropod dinosaurs that lived in what is now North America during the Early Jurassic, about 186 million years ago. Three skeletons were discovered in northern Arizona in 1940, and the two best preserved were collected in 1942.
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 ...
Illustration of the bones in the holotype. All specimens of Sarahsaurus were collected from the Lower Jurassic Kayenta Formation near Gold Spring, Arizona. [2] The genus is based on a nearly complete and articulated (with bones still connected to each other) skeleton with a fragmentary and disarticulated skull (holotype, specimen number TMM 43646-2).
Kolob Canyons from the end of Kolob Canyons Road. Stream erosion has incised the Kolob Plateau to form canyons that expose the red-orange colored Navajo Sandstone and other formations. The geology of the Zion and Kolob canyons area includes nine known exposed formations, all visible in Zion National Park in the U.S. state of Utah.
The Capitol Reef area was on the edge of an epicontinental sea for much of the Cretaceous (USGS). Early Cretaceous time brought continental deposition that was dominated by rivers to the area. Sandstones and mudstones accumulated to form the 0 to 166 foot (50.5 m) thick slope-forming Cedar Mountain Formation.
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