The Salt River is a river in Gila and Maricopa counties in Arizona, United States, that is the largest tributary of the Gila River. The river is about 200 miles (320 km) long. Its drainage basin covers about 13,700 square miles (35,000 km2). The longest of the Salt River's many tributaries is the 195-mile (314 km) Verde River. The Salt's headwaters tributaries, the Black River and East Fork, increase the river's total length to about 300 miles (480 km). The name Salt River comes from the river's course over large salt deposits shortly after the merging of the White and Black Rivers.
The Verde River is a major tributary of the Salt River in the U.S. state of Arizona. It is about 170 miles (270 km) long and carries a mean flow of 602 cubic feet per second (17.0 m3/s) at its mouth. It is one of the largest perennial streams in Arizona.
Canyon Lake is one of four reservoirs that were formed by the damming of the Salt River in the U.S. state of Arizona as part of the Salt River Project. It was formed by the Mormon Flat Dam, which was completed in 1925 after two years of construction. Canyon Lake, with a surface area of 950 acres (380 ha), is the third and smallest of the four lakes created along the river. Two others, Apache Lake and Roosevelt Lake, are upstream. The fourth, Saguaro Lake, is downstream.
Cottonwood Cove is situated at the banks of Lake Mohave on the Nevada-Arizona border in Clark County, Nevada, United States. It stands just 13.1 miles and 23 minutes east of Searchlight, 12.5 miles north of Laughlin and an hour away from Las Vegas. It is the site of the Cottonwood Cove Resort and Marina. The cove is part of the Lake Mead National Recreation Area administered by the U.S. National Park Service. The desert lake is approximately 67 miles long and is backed by the Davis Dam on the Colorado River.
Lynx Lake, Arizona, is a 55-acre (220,000 m2) reservoir located within Prescott National Forest, approximately 5 miles (8.0 km) east of Prescott, Arizona, in the Bradshaw Mountains. The lake is located at 5,530 feet (1,690 m) elevation and is stocked for fishing. It is one of the most popular recreation areas in central Arizona. Mild weather, the cool ponderosa pine forest, trout fishing, boating, mountain hiking, horseback riding, archaeological sites, and bird watching attract visitors from throughout Arizona. The lake was formed in 1952, when a dam was put in Lynx Creek, 6 miles (9.7 km) below Walker, Arizona.
San Carlos Lake was formed by the construction of the Coolidge Dam and is rimmed by 158 miles (254 km) of shoreline. The lake is located within the 3,000-square-mile (7,800 km2) San Carlos Apache Indian Reservation, and is thus subject to tribal regulations.
Apache Lake is one of four reservoirs built along the Salt River in central Arizona as part of the Salt River Project.
Theodore Roosevelt Lake is a large reservoir formed by Theodore Roosevelt Dam on the Salt River in Arizona as part of the Salt River Project (SRP). Located roughly 80 miles (130 km) northeast of Phoenix in the Salt River Valley, Theodore Roosevelt is the largest lake or reservoir located entirely within the state of Arizona. The reservoir and the masonry dam that created it, Roosevelt Dam, were both named after U.S. President Theodore Roosevelt who dedicated the dam himself on March 18, 1911. Roosevelt Lake is a popular recreation destination within the Tonto National Forest; the facilities located at this lake are managed by that authority.
Crown King is an unincorporated community in Yavapai County, Arizona, United States, located at an elevation of 5,771 feet (1,759 m). Crown King has a ZIP Code of 86343; in 2000, the population of the 86343 ZCTA was 133. The site of a former gold mining town, Crown King is 28 miles west of Interstate 17 on Senator Highway, high in the Bradshaw Mountains. The community is named after the Crowned King mine, but the name was shortened to Crown King in 1888. Horsethief Basin Lake resides 6.5 miles southeast of Crown King on Crown King Rd/Forest 259 Rd.
Goldwater Lake is a reservoir formed by a dam on Banning Creek, located south of Prescott in North Central Arizona. This lake is maintained by the City of Prescott Parks and Recreation Department. The park has facilities for picnicking, fishing, boating, hiking, volleyball, and horseshoes.
Watson Lake is one of two reservoirs at the Granite Dells, in Prescott, Arizona, that was formed in the early 1900s when the Chino Valley Irrigation District built a dam on Granite Creek. The City of Prescott bought the reservoir and surrounding land in 1997 to preserve it as recreational land. Local rockclimbers use the granite cliffs above and adjacent to the lake for top-roping and lead climbing. The lake is also the home of TriCity Prep Rowing Crew, a local high school team and only rowing team in Northern Arizona.
Built in 1928, Scott Reservoir is an irrigation impoundment on Porter Creek near Pinetop-Lakeside, Arizona, USA. The least developed of the "in town" lakes, trees surround Scott Reservoir. It lies just outside the town limits on the Apache-Sitgreaves National Forests.
Located in the heart of Pinetop-Lakeside, Woodland Lake and the park surrounding it have been called the town's "Crown Jewel." In addition to trout fishing, the lake provides a host of other outdoor recreation opportunities. Woodland Lake lies on city and Apache-Sitgraves National Forest property, just west of White Mountain Blvd. in Pinetop.
Fain Lake is a reservoir located near Prescott Valley in Yavapai County, North Central Arizona.
Granite Basin Lake is a reservoir located near Prescott, in Yavapai County, North Central Arizona. It is in the Prescott National Forest, adjacent to the Granite Mountain Wilderness Area.
Parker Canyon Lake is located in southeastern Arizona, 28 miles (45 km) southwest of Sierra Vista around the Huachuca Mountains and about 5 miles (8.0 km) north of the border with Mexico. The lake is a reservoir formed by a dam in Parker Canyon in the south end of the Canelo Hills in southwestern Cochise County. Parker Canyon is a tributary to the Santa Cruz River in the San Rafael Valley. The facilities are maintained by Coronado National Forest division of the USDA Forest Service.
Patagonia Lake is a man-made reservoir in Santa Cruz County, Arizona, United States, located southwest of the town of Patagonia, Arizona and northeast of Nogales. The lake was created by damming Sonoita Creek, and is a popular area for boating and sport fishing. Facilities are maintained by Arizona State Parks as part of Patagonia Lake State Park.
Roper Lake State Park is a state park of Arizona, surrounding 32-acre (130,000 m2) Roper Lake. The park is located off U.S. Route 191, 5 miles (8.0 km) south of Safford, at the Gila River and Valley.
Peña Blanca Lake is a reservoir in Arizona, United States, located 18 miles (29 km) northwest of Nogales. The facilities are maintained by the Coronado National Forest division of the USDA Forest Service. The lake was created in 1957 by the Arizona Game and Fish Department.Back then this lake was known for a plush resort that was located there. In 2008, the lake was closed to clean mercury contamination within the sediment, thought to be from old mines in the area. Also the former plush resort was removed as well. The lake was reopened in August 2009. In 2013, an Arizona Department of Environmental Quality report showed that mercury levels were similar to those before the lake was drained and dredged. One potential cause for the high mercury could be naturally occurring mercury seeping through the faults or a spring in the lake, though these claims are still under investigation.
Picacho Reservoir is just 11 miles (18 km) south of Coolidge in central Arizona, United States. The reservoir was built in the 1920s as part of the San Carlos Irrigation Project. The reservoir's original purpose was water storage and flow regulation for the Florence-Casa Grande and Casa Grande Canals. The lake's design capacity was 24,500 acre-feet (30,200,000 m3) of water, with a surface area of over 2 square miles (5.2 km2). Over the years, siltation and vegetation have reduced the capacity and surface area, so that much of the reservoir is a shallow marsh with extensive stands of cattails and rushes. Water level is highly variable, and the lake is completely dry in some years.
