Search results
Results from the WOW.Com Content Network
The Provo River (Ute: Timpanoquint, “Rock River) [4] is located in Utah County and Wasatch County, Utah, in the United States.It rises in the Uinta Mountains at Wall Lake and flows about 71 miles (114 km) southwest to Utah Lake at the city of Provo, Utah.
The reservoir supplies water for agricultural, municipal, and industrial use. Recreational activities on and around the reservoir include boating, fishing, camping, swimming and water skiing. [3] The Deer Creek Dam is the key structure of the Provo River Project managed by the U.S. Department of the Interior Bureau of Reclamation.
Snake Creek originates on the southeastern slope of Sunset Peak, about 3 miles (4.8 km) south of Brighton. [6] and flows southeast through Snake Creek Canyon, receiving Lavina Creek (from the left heading downstream) and other minor tributaries until it receives Pine Creek at the base on the canyon in Wasatch Mountain State Park.
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.
University of Utah Hospital: Salt Lake City: University of Utah: 585 Utah State Hospital: Provo: Utah Department of Human Services 324 Utah Valley Hospital: Provo: Intermountain Healthcare [1] 395 VA Hospital: Salt Lake City: United States Department of Veterans Affairs [23] 48 Valley View Medical Center: Cedar City: Intermountain Healthcare [1] 48
The canal carries about 400 million gallons of water to water users in Utah County at a maximum capacity of 612 cfs. [3] [4] The canal transports water from the Provo river, Deer Creek Reservoir, and Jordanelle reservoir. [4] The recreational trail known as the Murdock Canal Trail is located on top of the canal for 17 miles. [9]
Arrowhead Water, also known as Arrowhead Mountain Spring Water, is a brand of drinking water that is sold in the western United States, particularly in Idaho, Nevada, Arizona, Utah, Colorado, New Mexico, Northwestern United States, the Northwest, and in California. It is bottled from 13 springs throughout the Western United States.
Springs have also been observed on the ocean floor, spewing warmer, low-salinity water directly into the ocean. [2] Springs formed as a result of karst topography create karst springs, in which ground water travels through a network of cracks and fissures—openings ranging from intergranular spaces to large caves, later emerging in a spring.