Ottawa River

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This is about the river in Canada. For other uses, see Ottawa River (disambiguation).
Coordinates: 45°27′N 74°05′W / 45.45, -74.083
Ottawa River
River
none
Country Canada
Source Lake Capimitchigama
 - location Lac-Moselle, La Vallée-de-la-Gatineau RCM, Outaouais, Quebec
 - coordinates 47°36′N 75°48′W / 47.6, -75.8
Mouth Saint Lawrence River
 - location Montreal, Quebec
 - coordinates 45°27′N 74°05′W / 45.45, -74.083
Length 1,271 km (790 mi)
Basin 146,000 km² (56,371 sq mi)
Discharge for Carillon dam
 - average 1,950 /s (68,864 cu ft/s)
 - max 8,000 /s (282,517 cu ft/s)
 - min 700 /s (24,720 cu ft/s)
Map of the Ottawa River drainage basin
Map of the Ottawa River drainage basin

The Ottawa River (French: Rivière des Outaouais) is a river in the Canadian provinces of Ontario and Quebec. It defines for most of its length the border between these two provinces.

Contents

[edit] Geography

The river rises from its source in Lake Capimitchigama in the Laurentian Mountains of central Quebec, flows west to Lake Timiskaming, where it begins defining the interprovincial border with Ontario.

From Lake Timiskaming the river flows southeast to Ottawa and Gatineau where it tumbles over the Chaudière Falls and further takes in the Rideau and Gatineau Rivers.

The Ottawa River drains into the Lake of Two Mountains and the Saint Lawrence River at Montreal. The total length of the river is 1,271 km, and it drains an area of 146,000 km2, 65% in Quebec and the rest in Ontario. The average waterflow measured at Carillon dam, near the Lake of Two Mountains, is 1,950 m3/s, and it can vary from 700 to 8,000 m3/s.

Major tributaries include:

In this false-colour satellite image, the Ottawa River flows southeast, joining the Saint Lawrence River which flows northeast. Heavily forested areas appear differing shades of orange/red, while farmland is tan shades.

Communities along the Ottawa River include (in down-stream order):

[edit] Geology

Following the retreat of the glaciers from the area at the end of the last ice age, the Ottawa River valley was flooded by an arm of the Atlantic Ocean known as the Champlain Sea. Fossil remains of marine life have been found in marine clay formed during that time. Sediment deposits from this period have resulted in areas of poor drainage and the presence of large bogs in some ancient channels of this river. Another consequence was the formations of large deposits of a material commonly known as Leda clay; these deposits become highly unstable after heavy rains. Numerous landslides have occurred as a result. The former site of the town of Lemieux, Ontario collapsed into the South Nation River in 1993; however, the residents had already been relocated because of the suspected instability of the earth in that location.

Large numbers of Canada Geese, ducks, gulls and shorebirds take advantage of spring flooding and wetlands in the Ottawa River valley during migration. Ducks also overwinter in sections of the river that do not freeze over.

The Ottawa River lies in the Ottawa-Bonnechere Graben, which is a Mesozoic rift valley that formed 175 million years ago.

[edit] History

A railroad bridge over the Ottawa River in Mattawa, Ontario.

The river was an important trade route for the Algonquin people, who called it Kitchissippi, "Great River". Some early European explorers, possibly considering the Ottawa River to be more significant than the Upper Saint Lawrence River, applied the name River Canada to the Ottawa River and the Saint Lawrence River below the confluence at Montreal. As the extent of the Great Lakes became clear and the river began to be regarded as a tributary, it was variously known as the Grand River, "Great River" or Grand River of the Algonquins before the present name was settled upon. This name change resulted from the Ottawa peoples' control of the river circa 1685. However, only one band of Ottawa, the Kinouncherpirini or Keinouch, ever inhabited the Ottawa Valley.

In 1615, Samuel de Champlain and Étienne Brûlé, assisted by Algonquin guides, were the first Europeans to travel up the Ottawa River and follow the water route west to Georgian Bay. For the following two centuries, this route was used by French fur traders to Canada's interior.

In the early 19th century, the Ottawa River and its tributaries were used to gain access to large virgin forests of white pine. A booming trade in timber developed, and large rafts of logs were floated down the river. In 1832, the Ottawa River was connected to Lake Ontario via the Rideau Canal. Today, Outaouais Herald Emeritus at the Canadian Heraldic Authority is named after the river.

Several hydroelectric dams have been constructed on the river. However, it is still extensively used for recreational boating.

[edit] Hydroelectric installations

Hydroelectric installations on the Upper Ottawa (in downstream order):

Installation Type Generating cap. Year built Name of reservoir Operator
Bourque Dam Dam n/a 1949 Dozois Reservoir Hydro-Québec
Rapide-7 Generating station 48 MW 1941 / 1949 Decelles Lake Hydro-Québec
Rapide-2 Run of river g.s. 48 MW 1954 n/a Hydro-Québec
Rapides-des-Quinze Run of river g.s. 95 MW 1923 n/a Hydro-Québec
Rapides-des-îles Run of river g.s. 147 MW 1966 n/a Hydro-Québec
Première-Chute Run of river g.s. 130 MW 1968 n/a Hydro-Québec

Lower Ottawa (in downstream order):

Installation Type Generating cap. Year built Name of reservoir Operator
Otto Holden Run of river g.s. 243 MW 1952 n/a Ontario Power Generation
Des Joachims Run of river g.s. 429 MW 1950 Holden Lake Ontario Power Generation
Bryson Run of river g.s. 61 MW 1925 n/a Hydro-Québec
Chenaux Run of river g.s. 144 MW 1950 n/a Ontario Power Generation
Chute-des-Chats (Chats Falls) Run of river g.s. 185 MW 1931 Lac des Chats Hydro-Québec and OPG *
Hull-2 Run of river g.s. 27 MW 1920 n/a Hydro-Québec
Carillon Run of river g.s. 752 MW 1962 n/a Hydro-Québec

* ) Ontario Power Generation operates generators 2, 3, 4, and 5 with a capacity of 96 MW; and Hydro Quebec operates generators 6, 7, 8, and 9 with a capacity of 89 MW.

[edit] See also

[edit] External links

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