South Fork Salmon River

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South Fork Salmon River
SFSalmon.jpg
Rafters on the South Fork Salmon River
Country United States
State Idaho
Tributaries
 - left Secesh River
 - right East Fork, Elk Creek
Source near Monumental Peak
 - location Salmon River Mountains, Valley County
 - elevation 7,600 ft (2,316 m)
 - coordinates 44°28′47″N 115°41′06″W / 44.47972°N 115.68500°W / 44.47972; -115.68500 [1]
Mouth Salmon River
 - location near Mackay Bar, Idaho County
 - elevation 2,146 ft (654 m)
 - coordinates 45°22′40″N 115°30′47″W / 45.37778°N 115.51306°W / 45.37778; -115.51306Coordinates: 45°22′40″N 115°30′47″W / 45.37778°N 115.51306°W / 45.37778; -115.51306 [1]
Length 86 mi (138 km) [2]
Basin 1,309 sq mi (3,390 km2) [3]
Discharge for Mackay Bar
 - average 1,983 cu ft/s (56 m3/s) [3]
 - max 21,600 cu ft/s (612 m3/s)
 - min 318 cu ft/s (9 m3/s)
Salmonrivermapfinal.jpg
Map showing the Salmon River basin. The South Fork is the second major tributary from left.

The South Fork Salmon River is an 86-mile (138 km)[2] tributary of the Salmon River in Idaho and Valley Counties in central Idaho.[1] The river drains a rugged, lightly populated wilderness watershed in the Salmon River Mountains. It is the second-largest tributary of the Salmon River, after the Middle Fork.

Geography[edit]

Beginning near 7,902-foot (2,409 m) Monumental Peak in the Boise National Forest, the river flows generally north to its confluence with the Salmon near Mackay Bar, about 135 miles (217 km) above the larger river's mouth on the Snake River. About midway along its course, it is joined by its two main tributaries – the East Fork South Fork Salmon River from the east, and the Secesh River from the west.[4] The river receives runoff from a total of 1,309 square miles (3,390 km2) of land, ranging in elevation from 9,322 feet (2,841 m) at North Loon Mountain to 2,146 feet (654 m) at the mouth of the river.[3]

History[edit]

The Native Americans living along the river were the Nez Perce, Shoshone, Bannock and Paiute. The river and its valley were used largely as a place for fishing, hunting and gathering, while local hot springs provided camping sites during the winter.[5]

The first recorded Europeans to see the South Fork may have been a group of mountain men working under the American Fur Company in 1831. They crossed the upper part of the river while reconnoitering the western part of the Salmon River system for good beaver streams.[6] In the 1860s, prospectors discovered gold on the South Fork, leading to the initial settlement of the drainage by Westerners. After the gold rush faded, a few of the miners stayed on as homesteaders and ranchers.[5]

The drainage was heavily logged from the 1940s to the mid-1960s, when an estimated 320 million board feet of timber was taken from the basin. More than 800 miles (1,300 km) of logging roads were constructed across the drainage.[5]

Ecology[edit]

The South Fork is an important habitat for Chinook salmon, Westslope cutthroat trout, bull trout and steelhead trout and has been designated a critical habitat for salmon. Although aquatic habitat in the South Fork drainage is considered good as a whole, some tributaries have been damaged by logging, mining and road-building activities, which has increased the sediment load in the river. About 340 miles (550 km) of backcountry roads in the drainage have been decommissioned and are undergoing restoration by the U.S. Forest Service.[5][7]

Plant communities in the South Fork drainage range from grassland and shrubland, Ponderosa pine, Douglas fir and Grand fir forests at lower elevations, to subalpine fir, lodgepole pine, whitebark pine and aspen at mid to high elevations.[7] Among large mammals, the watershed is home to Rocky Mountain elk, white-tailed deer, mule deer, black bear, cougar, mountain goat, bighorn sheep and gray wolf. The area has over 200 confirmed species of resident and migratory birds.[5]

Hydrology[edit]

The United States Geological Survey (USGS) operated a stream gage at the mouth of the South Fork between 1993 and 2003, recording an annual mean of 1,983 cu ft/s (56.2 m3/s). The highest annual mean was 3,125 cu ft/s (88.5 m3/s) in 1997, and the lowest was 869.9 cu ft/s (24.63 m3/s) in 2001. Mean monthly discharge rates for the South Fork are displayed in the below graph.

Monthly discharges at Mackay Bar (cfs)[3]

Recreation[edit]

Although not as frequently run as the Middle Fork, the South Fork is also well known for challenging whitewater. Boaters frequently put in at the Secesh River, about 37 miles (60 km) above the mouth of the South Fork on the main stem Salmon. Because of their relatively pristine condition, the South Fork and its tributary the Secesh are being considered for inclusion in the National Wild and Scenic Rivers system.[7]

See also[edit]

References[edit]

  1. ^ a b c "South Fork Salmon River". Geographic Names Information System. United States Geological Survey. 1979-06-21. Retrieved 2013-12-15. 
  2. ^ a b "USGS National Atlas Streamer". United States Geological Survey. Retrieved 2013-12-15. 
  3. ^ a b c d "USGS Gage #13314900 on the South Fork Salmon River at Mouth near Mackay Bar, ID". National Water Information System. United States Geological Survey. 1993–2003. Retrieved 2013-12-15. 
  4. ^ USGS Topo Maps for United States (Map). Cartography by United States Geological Survey. ACME Mapper. Retrieved 2013-12-15. 
  5. ^ a b c d e "South Fork Salmon River Information". Payette National Forest. United States Forest Service. Retrieved 2013-12-15. 
  6. ^ "Exploration and Settlement of Salmon River" (PDF). Idaho State Historical Society Reference Series. Idaho State Historical Society. ? (242). November 1965. 
  7. ^ a b c "Management Area 12: South Fork Salmon River" (PDF). United States Forest Service. Retrieved 2013-12-15.