South Fork San Joaquin River | |
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![]() South Fork below Florence Lake | |
Location | |
Country | United States |
State | California |
Physical characteristics | |
Source | Martha Lake (California) |
• location | Kings Canyon National Park |
• coordinates | 37°05′39″N118°43′16″W / 37.09417°N 118.72111°W /37.09417; -118.72111[1] |
• elevation | 11,010 ft (3,360 m) |
Mouth | San Joaquin River |
• location | Ansel Adams Wilderness |
• coordinates | 37°26′13″N119°14′36″W / 37.43694°N 119.24333°W /37.43694; -119.24333[1] |
• elevation | 3,704 ft (1,129 m) |
Length | 48 mi (77 km)[2] |
Discharge | |
• location | Hoffman Meadow[3] |
• average | 456 cu ft/s (12.9 m3/s)[4] |
• minimum | 8.5 cu ft/s (0.24 m3/s) |
• maximum | 5,930 cu ft/s (168 m3/s) |
TheSouth Fork San Joaquin River is the largestheadwater of theSan Joaquin River in centralCalifornia,United States. About 48 miles (77 km) long,[2] it drains an area of the highSierra Nevada about 60 miles (97 km) northeast ofFresno.
The South Fork begins at Martha Lake, 11,010 ft (3,360 m) above sea level,[5] nearMount Goddard in the northern section ofKings Canyon National Park inFresno County. It flows northwest through the narrow Goddard Canyon, receiving Evolution Creek from the east, then leaves the park at the confluence with Piute Creek from the north, entering theSierra National Forest. It then flows west, through Blayney Meadows, into Florence Lake, impounded byFlorence Lake Dam. Below the dam it flows briefly north, receiving Bear Creek, before turning west again, through a wider valley pastMono Hot Springs then receiving its main tributary, Mono Creek, from the north. The South Fork enters theAnsel Adams Wilderness as it turns northwest, receiving Four Forks and Rube Creeks before crossing intoMadera County. Soon after entering Madera County, it joins the San Joaquin River, in a deep granite canyon below Balloon Dome at San Joaquinriver mile 334 (km 537), a short distance aboveMammoth Pool Reservoir.[6]
The Florence Lake Dam, as well as Vermillion Valley Dam on Mono Creek which formsLake Thomas A. Edison, are both part of theBig Creek Hydroelectric Project operated bySouthern California Edison to provide electricity toLos Angeles. In 1925, water was first diverted from the South Fork via the Ward Tunnel intoHuntington Lake. The concrete multiple-arch Florence Lake dam was completed in 1926 to ensure a year-round water supply for the tunnel. The larger, earthen Vermillion Valley Dam was built much later, in 1953. The dams divert a considerable amount of water from the South Fork for power generation, especially during the late summer and fall when water flows are already naturally low.
The South Fork between Piute Creek and Florence Lake has a wide variety of difficulty levels for boating, ranging from a gentle, smooth meandering stream in the Blayney Meadows section to continuousClass VI to V+ whitewater in the last 2 miles (3.2 km) above Florence Lake, as well as a number of waterfalls that must be portaged. Below the Florence Lake Dam river flows are less reliable due to water diversions, except in years of particularly heavy snowmelt.[7]