Redstone River

Redstone River
Country Canada
Basin features
Main source Redstone Plateau
1,068 m (3,504 ft)
River mouth Mackenzie River
133 m (436 ft)
64°17′10″N 124°32′40″W / 64.28611°N 124.54444°W / 64.28611; -124.54444Coordinates: 64°17′10″N 124°32′40″W / 64.28611°N 124.54444°W / 64.28611; -124.54444[1]
Progression Southwest-northeast
Basin size 16,400 km2 (6,300 sq mi)
Tributaries
  • Left:
    Moose Horn River, Parallel Creek
  • Right:
    Ravens Throat River
Physical characteristics
Length 289 km (180 mi)
Discharge
  • Average rate:
    139 m3/s (4,900 cu ft/s)

The Redstone River is a large river in the Northwest Territories of Canada. It is about 289 kilometres (180 mi) long.[2] It is a tributary of the Mackenzie River, joining it on the left bank some 100 kilometres (62 mi) north of Wrigley. Draining a rugged and high area of the Mackenzie Mountains, the Redstone watershed is sparsely populated by people but remains an ecological haven for wildlife including moose, caribou, wolves Dall's Sheep and Bears. It is a pristine mountain wilderness.

Course

It begins in several ponds on Rockslide Pass south of the Redstone Plateau deep within the Mackenzie Mountains, at an elevation of 1,068 metres (3,504 ft). The river initially flows northwest, turning west where the Moose Horn River enters from the left. It makes a bend to the north, turning south near Wrigley Lake, and receives its larger tributary, the Ravens Throat River, as it cuts through the Redstone Range. The Redstone turns north, bending west around the Silvan Plateau, leaving its canyon and spreading onto the plains surrounding the Mackenzie River, which it joins about 40 kilometres (25 mi) after that point, at just 133 metres (436 ft) above sea level, 13 kilometres (8 mi) upstream from the Keele River.[3]

Watershed

The Redstone's watershed encompasses an area of roughly 16,400 km2 (6,300 sq mi).[4] Its average annual discharge, measured at a gauge near the mouth from 1963 to 1974, was roughly 139 cubic metres per second (4,900 cu ft/s). The highest monthly flows occurred in August at 454 cubic metres per second (16,000 cu ft/s), and the lowest was 15.7 cubic metres per second (550 cu ft/s) in March, because of its dependence on glacier and snow melt in the brief Arctic summer. The highest recorded flow was 545 cubic metres per second (19,200 cu ft/s) in July 1968, and the lowest was 11.3 cubic metres per second (400 cu ft/s) in February 1972.[4] Its tributary, the Ravensthroat River, has the odd distinction of being significantly larger than the Redstone at their confluence. Older maps referred to these rivers as the North and South Redstone respectively.

Recreation

Recently, both the Redstone and Ravensthroat Rivers have proven to be challenging and rewarding multiday canoe/rafting expeditions, with many class 2 and 3 rapids and canyons in a remote montane wilderness setting. The first modern descent of the Redstone was in the year 2000 via the Raven's Throat tributary by a National Geographic Explorers League group. Outfitters from the NWT and BC have since run guided trips down the rivers flying with a float plane into either Wrigley Lake for the Redstone or Divide Lake for the Raven's Throat (helicopter support required). The river and its tributaries offers a different experience compared to the other Makenzie Mountain rivers as it cuts through a unique geological area known as the Redstone Plateau. Trips usually last between 10–16 days long depending on the route, and finish in the communities of Tulita or Norman Wells on the Makenzie River.

See also

References

  1. Gazetteer of the Northwest Territories
  2. Length measured in Google Earth using data from Canadian topographic maps to find the source; source location is approximate
  3. Topo Maps for United States and Canada (Map). Cartography by U.S. and Canada, various sources. ACME Mapper. Retrieved 2010-05-01.
  4. 1 2 "Redstone River near the Mouth". Mackenzie Watershed. R-ArcticNET. 1963–1974. Retrieved 2010-05-04.
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