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Top Attractions in Santa Catalina Mountains

Mount Lemmon Ski Valley

Mount Lemmon Ski Valley is a recreational ski area in the U.S. state of Arizona, and the southernmost ski destination in the continental United States. Mount Lemmon Ski Valley is located on the slopes of Mount Lemmon in the Santa Catalina Mountains just north of Tucson, Arizona. It is part of the Coronado National Forest, located near the mountaintop village of Summerhaven. The summit is 9,157 feet above sea level, and receives approximately 180 inches of snow annually. Winter storms on Mount Lemmon are frequent, leaving untouched powder areas. The ski season on Mount Lemmon usually occurs between mid-December and April. The weather is usually mild enough to ski in a sweater and denim jeans, with temperatures ranging from 20 to 50 degrees Fahrenheit. There is no grooming at Mount Lemmon, which makes even the mild terrain challenging. Ski Valley is accessible via the Catalina Highway. Parking is limited at the ski area. The ski area is regularly closed some weekdays even when they have snow, but the specific days of closure vary. The highway is frequently closed for a day or so following substantial snowfalls until plows can clear the road. Restrictions limiting travel to vehicles with chains or four-wheel-drive above certain elevations may also be in effect during these times. The "back" road to Mount Lemmon from the town of Oracle, Arizona is dirt and is closed from December through March, and so provides no access during the ski season. The ski lift runs year round, as a "Sky Ride" experience in the summertime, offering views of the Ski Valley area, forest and grass-covered slopes, and the long distance vistas of the mountains and valleys in the distance north of the Santa Catalinas.

Pusch Ridge Wilderness Area

Pusch Ridge Wilderness Area is a 56,430 acre wilderness area. It is located within the Coronado National Forest in the Santa Catalina Mountains north of Tucson, Arizona, United States. Established in 1978, the area varies greatly in elevation and biodiversity, rising from 2,800 feet to over 9,100 feet in elevation. The area was originally created in an ill-fated effort to preserve and protect the sensitive Desert Bighorn Sheep population on Pusch Ridge, one of the last remaining populations in Arizona. Due in part to increased residential and commercial development around the Santa Catalina Mountains in Oro Valley and the Catalina Foothills, however, the Desert Bighorn Sheep population in the wilderness area has dwindled dramatically, and sightings have nearly ceased in recent years. In November 2013, 31 adult bighorn sheep were reintroduced to the area. In early February 2014, 2 lambs were spotted by an Arizona Game and Fish Department official. These two are the first Catalina-born desert bighorn sheep in nearly 25 years. Plant life at lower elevations includes saguaro cactus and other desert plants. Trees found at mid-level elevations include mountain mahogany, juniper and pinyon pine. Forests of fir and aspen grow above 8,000 feet. In the middle of the Santa Catalina mountains there is a dome-shaped core of Catalina granite, formed in the Triassic period. The south face of the mountains is formed by Catalina gneiss with bands of white quartzite, this face is the form of a steep anticline and it is separated from the rest of the mountains by a series of valleys.

Cañada del Oro

The Cañada del Oro, is a primary watershed channel in the valley of Tucson, Arizona, USA. The word cañada has a tilde and is pronounced in Spanish; in English it is pronounced kə-NYAH-də, not like the country of Canada. The Cañada del Oro originates in the remote Canyon del Oro in the Santa Catalina Mountains north of Tucson, fed by rainfall and melted snow from the northern face of Mount Lemmon and flows northward toward the town of Oracle. The Cañada del Oro is a perennial creek in Canyon del Oro while at higher altitudes. The Cañada del Oro curves from flowing northward to southward through the town of Oro Valley north of Tucson, where it is usually a dry riverbed. In Oro Valley the Cañada del Oro collects watershed from the western face of the Santa Catalina Mountains. The Cañada del Oro ultimately feeds into the Santa Cruz River just northwest of Tucson, the principal watershed channel in the Tucson valley. Historically, the Cañada del Oro was the focus of significant interest in gold mining, beginning with Spanish explorers in the 17th century. As early as 1880, the Cañada del Oro was labeled "Gold Cañon Creek" on American maps. Following the Mexican-American War, American gold-rushers continued the search for the valuable mineral through the 1930s. Prospectors discovered minimal amounts of gold in the Cañada del Oro through placer mining operations, and reportedly mined gold in the lost Mine with the Iron Door. The lost mine is the subject of a novel of the same name written by Harold Bell Wright in 1923.

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