Search results
Results from the WOW.Com Content Network
The San Rafael River is a tributary of the Green River, approximately 90 miles (140 km) long, in east central Utah, United States. [1] The river flows across a sparsely populated arid region of the Colorado Plateau, and is known for the isolated, scenic gorge through which it flows.
The Atuel River flows through the base of the canyon and contains several rapids, which are used for rafting and canoeing. Those rapids are classified between class II (novice) and IV (advanced) in the International Scale of River Difficulty. [3] The surrounding area includes many hotels, camping sites, country clubs and other lodging ...
Emery, Grand, San Juan, Wayne Green River: Lambs Canyon: Salt Lake Lambs Canyon Road Little Cottonwood Canyon: Salt Lake Little Cottonwood Creek: SR-210: Little Emigration Canyon: Morgan Mormon Trail: Little Grand Canyon: Emery San Rafael River: Logan Canyon: Cache Logan River: US-89: Maple Canyon: Sanpete Maple Canyon: Utah Maple Canyon Road ...
Watershed of the Colorado River. The Colorado River is a major river in the Western United States, emptying into the Gulf of California.Rivers are listed upstream by the point they empty into the Colorado.
The main population of the county lives along the base of these mountains. The San Rafael Swell occupies most of the area to the east. The San Rafael Reef. The western side of the county is the most populated and contains numerous small communities residing in an agricultural valley that roughly parallels the Manti National Forest to the west.
Until the 1990s, it was the only bridge crossing the river. It no longer carries automobile traffic, but it is still open for pedestrian use. [2] It was added to the NRHP June 3, 1996. [3] San Rafael Bridge, October 2009
The San Rafael Swell is a large geologic feature located in south-central Utah, United States about 16 miles (26 km) west of Green River. The San Rafael Swell, measuring approximately 75 by 40 miles (121 by 64 km), consists of a giant dome-shaped anticline of sandstone, shale, and limestone that was pushed up during the Paleocene Laramide ...
Approximately 75 miles (120 km) long, it is the distinctive eastern edge of the San Rafael Swell. Composed primarily of steeply tilted layers of Navajo and Wingate Sandstone, it has been eroded into tall fins, domes, cliffs, and deep canyons. The San Rafael River, Interstate 70, and Muddy Creek all cut through the San Rafael Reef. There are ...