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Coyote Gulch is a tributary of the Escalante River, located in Garfield and Kane Counties in southern Utah, in the western United States.Over 25 mi (40 km) long, [1] Coyote Gulch exhibits many of the geologic features found in the Canyons of the Escalante, including high vertical canyon walls, narrow slot canyons, domes, arches, and natural bridges.
Robert B. Keiter, Sarah B. George and Joro Walker (editors), Visions of the Grand Staircase–Escalante: Examining Utah's Newest National Monument (Utah Museum of Natural History and Wallace Stegner Center, 1998) ISBN 0-940378-12-4; Julian Smith, "Moon Handbooks Four Corners" (Avalon Travel Publishing, 2003) ISBN 1-56691-581-3
Ruth DeEtte Simpson (May 6, 1918 – January 19, 2000) [1] was an American archaeologist and founder of the Archaeological Survey Association of Southern California. [2]Born in Pasadena, California, Simpson received her master's degree from the University of Southern California in 1944 and went on to be the curator of the Heard Museum in Arizona for two years. [3]
The lower section of the river, southeast of Coyote Gulch, is now beneath the surface of Lake Powell. Numerous side canyons also feed the main river, accounting for the large size of the basin. From the west, the major tributaries are Harris Wash , Twentyfive Mile Creek, Coyote Gulch, Fortymile Gulch , and Fiftymile Creek, along with the ...
The Wahweap Formation of the Grand Staircase–Escalante National Monument is a geological formation in southern Utah and northern Arizona, around the Lake Powell region, whose strata date back to the Late Cretaceous (Campanian stage).
(1994) "Hole-in-the-Rock Trail" article in the Utah History Encyclopedia. The article was written by Encyclopedia staff and the Encyclopedia was published by the University of Utah Press. ISBN 9780874804256. Archived from the original on March 22, 2024 and retrieved on May 13, 2024.
Traditionally, the Kaiparowits Formation has been considered to be roughly equivalent in age to the northern Dinosaur Park Formation.This, combined with the differences in fauna between the two formations, has led some scientists, most notably Scott Sampson, to conclude that there was some barrier separating northern and southern Laramidia at this time.
Coyote Gulch is also confused with another stream in the area of Baker Beach and China Beach Division. The division, which is constantly changing due locals and kids digging, natural phenomenon. Lobos Creek is the Presidio's primary source of potable water.