Search results
Results from the WOW.Com Content Network
The Little Cottonwood stock is a granitic intrusion that extends from the mouth of the canyon almost to Snowbird ski resort. It is Oligocene in age, roughly 30.5 to 29 million years old, composed primarily of granodiorite, quartz monzonite, and granite, with some mafic enclaves.
Little Cottonwood Creek is one of the principal streams entering Salt Lake Valley from the east. The creek rises near the summit of the Wasatch Mountains, a short distance south of the ski resort town of Alta, and flows in a westerly direction through Little Cottonwood Canyon until it emerges into Salt Lake Valley about eleven miles from its source.
State Route 210 (SR-210) is a state route in the U.S. state of Utah that is the access road for Little Cottonwood Canyon and the ski resorts of Alta and Snowbird.The 13.62 mi (21.92 km) highway straddles the southeastern edge of the Salt Lake Valley before it enters the mouth of Little Cottonwood Canyon.
Snowbird, Utah. The development of Little Cottonwood Canyon and the town of Alta dates to the 19th century. A U.S. Army soldier first prospected for silver there in 1869. Mining became a large local industry, and Little Cottonwood Canyon became one of the largest producers of silver ore in the Wasatch Mount
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.
Alta was founded about 1865 to house miners from the Emma mine, the Flagstaff mine, and other silver mines in Little Cottonwood Canyon. Sensationally rich silver ore in the Emma mine enabled its owners to sell the mine at an inflated price to British investors in 1871.
Alta ski resort in Little Cottonwood Canyon, February 2009. In addition to ski resorts, there are hundreds of miles of mountain biking and hiking trails winding through the canyons and alpine valleys of the Wasatch Range. These offer backcountry access close to a large metropolitan area.
An obvious and prominent east-facing chute seen from Little Cottonwood Canyon, this line has been known by a few names, but is most commonly referenced as Suicide Chute. [8] This descent has slopes upwards of 40° and is rated S4. [6]