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Big Cottonwood Canyon: Salt Lake Big Cottonwood Creek: SR-190: Bingham Canyon: Salt Lake Bingham Creek: SR-209: Savage Bingham and Garfield Railroad (ex-D&RGW) Bluejohn Canyon: Wayne site of Aron Ralston's accident Box Elder Canyon: Box Elder Box Elder Creek: US-91: Butterfield Canyon: Salt Lake Butterfield Creek: Butterfield Canyon Road ...
Emigration Canyon is a city and canyon in Salt Lake County, Utah, United States, located east of Salt Lake City in the Wasatch Range. Beginning at the southern end of the University of Utah, the canyon itself heads east and northeast between Salt Lake City and Morgan County. Its boundaries do not extend to the county line, nor do they encompass ...
A snowy winter view of the canyon Lake Blanche in Big Cottonwood Canyon, c. 1869. Big Cottonwood Canyon is a canyon in the Wasatch Range 12 miles (19 km) southeast of Salt Lake City in the U.S. state of Utah. [2] The 15-mile (24 km)-long canyon provides hiking, biking, picnicking, rock-climbing, camping, and fishing in the summer.
The average water yield of Big Cottonwood Creek is 52,864 acre-feet (65,207,000 m 3), which is the highest water yield of any Wasatch Front canyon stream in Salt Lake County. This canyon is a protected watershed area under strict management controls since it is a major source of drinking water for Salt Lake City. No dogs or horses are allowed.
Parleys Canyon begins where I-215 merges into I-80 in Salt Lake City and ends at Parleys Summit. The lower part of the canyon is relatively twisty and narrow and had to be dynamited to make way for I-80. Despite this, the interstate remains six or more lanes wide throughout the canyon; it is built over Parleys Creek in many places.
The canyon is part of Granite, a CDP and "Community Council" designated by Salt Lake County. The canyon is a glacial trough (U-shaped canyon), carved by an alpine glacier during the last ice age, 15,000 to 25,000 years ago. A number of rare and endemic plant species are found in the canyon's Albion Basin.
Millcreek Canyon. Millcreek Canyon (also Mill Creek Canyon) [1] (Shoshoni: Tempin-Tekkoappah, “rock trap”) [2] is a canyon in the Wasatch Mountains and part of Millcreek City on the east side of the Salt Lake Valley, Utah. It is a popular recreation area both in the summer and in the winter. [3]
Granite Mountain is a mass of solid rock one mile up Little Cottonwood Canyon in the Wasatch Range of Utah, not too far from Salt Lake City, Utah.Despite its name, Granite Mountain is primarily composed of quartz monzonite, an igneous rock similar to granite in appearance, physical characteristics, and chemical composition.
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