Capousacataca River

The Capousacataca River is a tributary of the Mégiscane River, flowing into the north-eastern part of Senneterre in La Vallée-de-l'Or Regional County Municipality (RCM), in the administrative region of Abitibi-Témiscamingue, in Quebec, Canada.

Capousacataca
Watershed of Nottaway River
Location
CountryCanada
ProvinceQuebec
RegionAbitibi-Témiscamingue
Physical characteristics
SourceLeigne Lake
 • locationSenneterre, La Vallée-de-l'Or Regional County Municipality (RCM), Abitibi-Témiscamingue, Quebec
 • coordinates48°40′06″N 76°09′33″W
 • elevation389 m (1,276 ft)
MouthMégiscane River
 • location
Senneterre, La Vallée-de-l'Or Regional County Municipality, Abitibi-Témiscamingue, Quebec
 • coordinates
48°30′37″N 76°25′05″W
 • elevation
385 m (1,263 ft)
Length17.4 km (10.8 mi)[1]
Basin features
Tributaries 
 • left
  • (upstream)
  • outlet of lake Kanijokamacik
  • outlet of lake Tremblay
  • outlet of a set of lakes including Akokodjic and Palazo
  • outlet of lake Goulish.
 • right
  • (upstream)
  • outlet of lake Nibiciwâbo
  • outlet of lake Nibomimakizin.

The course of the river successively crosses the townships of Charrette and Girouard.

The Capousacataca River runs entirely on forest land north-east of the La Vérendrye Wildlife Reserve and on the west side of Gouin Reservoir. Forestry is the main economic activity of this hydrographic slope; recreational tourism activities, second. The surface of the river is usually frozen from the beginning of December to the end of April. The hydrographic slope of the Capousacataca River is served by the R0808 forest road that goes up this valley (first on the west side, then on the east side) to the south east of Charrette Lake, where the road is oriented towards the North -East.

Geography
The Capousacataca River originates near the northern limit of the Abitibi-Témiscamingue administrative region at the mouth of lac Valets.

The mouth of this lake is located at the bottom of a Northeast bay at:

  • 7.4 kilometres (4.6 mi) north of the confluence of the Capousacataca River with the Mégiscane River;
  • 53.8 kilometres (33.4 mi) north-east of the confluence of the Mégiscane River with Parent Lake (Abitibi);
  • 40.7 kilometres (25.3 mi) north of the Canadian National Railway's Paradise Station;
  • 64.7 kilometres (40.2 mi) north-east of Senneterre.

The main hydrographic slopes near the Capousacataca River are:

From the mouth of Lake Valets, the Capousacataca River flows over 17.4 kilometres (10.8 mi) according to the following segments:

  • 5.2 kilometres (3.2 mi) northeasterly, forming a westerly curve to the north shore of a lake formed by a widening of the river;
  • 2.5 kilometres (1.6 mi) north, then south, across a lake (length: ; altitude: 390 metres (1,280 ft)) formed by the widening of the river to its mouth;
  • 1.1 kilometres (0.68 mi) southerly crossing Miglet Lake (length: 1.9 kilometres (1.2 mi); altitude: 378 metres (1,240 ft));
  • 8.6 kilometres (5.3 mi) south by cutting off forest road R0808 to the confluence of the river[2]

The Capousacataca River discharges on the west bank of a bend of the Mégiscane River. The latter usually flows westward, forming a large hook to the south. It is a tributary of the east shore of Parent Lake (Abitibi). The latter empties into the Bell River, a tributary of Matagami Lake which in turn flows into the Nottaway River, a tributary of the southeastern shore of the James Bay.

This confluence of the Capousacataca River with the Mégiscane River is located upstream of Lake Girouard. More specifically, the Capousacataca River flows to:

  • 52.8 kilometres (32.8 mi) north-east of the confluence of the Mégiscane River with Parent Lake (Abitibi);
  • 30.6 kilometres (19.0 mi) northwest of the Foresyth railway stop on the Canadian National Railway;
  • 63.3 kilometres (39.3 mi) north-east of the village center of Senneterre;
  • 73.4 kilometres (45.6 mi) south-east of the village center of Lebel-sur-Quévillon;
  • 2.4 kilometres (1.5 mi) east of a bay on the east shore of lake Valets;
  • 71.9 kilometres (44.7 mi) west of Gouin Reservoir.

Toponymy

The hydronym "Capousacataca River" is of Native origin of the Algonquin nation, meaning "where there is a lot of dry wood". This toponym is indicated on a cartographic document dated 1940.

The toponym "Capousacataca River" was formalized on December 5, 1968, at the Commission de toponymie du Québec.[3]

gollark: This is ridiculous: ```local function cost(i) [lua junk here] endlocal function craft(i) [blablabla] cost(i) [blablabla] end -- that cost call errors about calling a nil value```
gollark: No, the problem is that you can't trust the client.
gollark: <@184468521042968577> Well, you could mine for a little bit then stop as a benchmark. The issue is that you can just send "Hash rate: 82 octillion" and get all the krist.
gollark: Maybe all particles on SC are just generated by a lone, overtaxed turtle.
gollark: Buy Ender Particle turtles for just 7KST extra with your order of a Synthetic Dragon Egg!

See also

References
  1. "Atlas of Canada". atlas.nrcan.gc.ca. Retrieved 2018-01-27.
  2. River segments measured from the Atlas of Canada (published on the Internet) from the Department of Natural Resources Canada.
  3. Commission de toponymie du Quebec - Bank of Place Names - Toponym: "Capousacataca River"
This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.