- This is about the river in Canada. For other uses,
see Ottawa River
.
The
Ottawa River (French: Rivière des
Outaouais) (Algonquin: Kichisìpi) is a river in the
Canadian provinces of Ontario
and Quebec
. It
defines for most of its length the border between these two
provinces.
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 St. Lawrence River
at Montreal
. The total length of the river is ; it
drains an area of 146,300 km
2, 65% in Quebec and
the rest in Ontario, with a mean discharge of 1,950
m
3/s.
The average annual mean waterflow measured at
Carillon
dam
, near the Lake of Two Mountains, is 1,939
m3/s, with average annual extremes of 749 to 5,351
m3/s. Record historic levels since 1964 are a low
of 529 in 2005 and a high of 8190 m
3/s in 1976.
Major tributaries include:
Communities along the Ottawa River include (in down-stream order):
- Notre-Dame-du-Nord, Quebec

- Ville-Marie, Quebec

- Témiscaming, Quebec

- Mattawa, Ontario

- Deux Rivières,
Ontario
- Rapides-des-Joachims, Quebec

- Laurentian Hills, Ontario

- Deep River, Ontario

- Sheenboro, Quebec

- Petawawa, Ontario

- Pembroke, Ontario

- Westmeath, Ontario

- Waltham, Quebec

- Fort-Coulonge, Quebec

- La Passe, Ontario

- Campbell's Bay, Quebec

- Portage-du-Fort, Quebec

- McNab/Braeside, Ontario

- Arnprior, Ontario

- Quyon, Quebec

- Aylmer, Quebec

- Hull, Quebec
- Ottawa,
Ontario

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- Gatineau,
Quebec

- Orléans, Ontario

- Masson-Angers, Quebec
- Clarence-Rockland, Ontario

- Thurso, Quebec

- Plaisance, Quebec

- Papineauville, Quebec

- Montebello, Quebec

- Fassett, Quebec

- L'Orignal, Ontario

- Grenville, Quebec

- Hawkesbury, Ontario

- Carillon,
Quebec

- Saint-André-Est, Quebec

- Rigaud, Quebec

- Saint-Placide, Quebec

- Hudson, Quebec

- Oka, Quebec

- Vaudreuil-sur-le-Lac, Quebec

- Vaudreuil-Dorion, Quebec

- Pincourt, Quebec

- Pointe-des-Cascades, Quebec

|
Geology
The Ottawa River lies in the
Ottawa-Bonnechere Graben, which is
a
Mesozoic rift
valley that formed 175 million years ago.
Following the retreat
of the glaciers from the area at the end of
the last ice age, the 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
shorebird 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.
History

An Algonquin Family
As it does to this day, the river played a primordial role in life
of the
Algonquin people, who lived
throughout its watershed at contact. The river is called
Kichisìpi, meaning "Great River" in
Anicinàbemowin, the
Algonquin language. The Algonquin define
themselves in terms of their position on the river, referring to
themselves as the Omàmiwinini, 'down-river people'. Although a
majority of the Algonquin First Nation lives in Quebec, the entire
Ottawa Valley is Algonquin traditional territory. Present
settlement is a result of adaptations made as a result of settler
pressures.
early European explorers, possibly considering the Ottawa River to
be more significant than the Upper St. Lawrence River, applied the
name
River Canada to the Ottawa River and the St. 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 people' 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 along the Mattawa and French Rivers to the Great Lakes
. For the following two centuries, this route
was used by French
fur traders and voyageurs to Canada's
interior. The river posed serious hazards to these
travelers. The section near
Deux Rivières used to have
spectacular and wild rapids, namely the
Rapide de la
Veillée, the
Trou, the
Rapide des Deux
Rivières, and the
Rapide de la Roche Capitaine. In
1800, explorer Daniel Harmon reported 14 crosses marking the deaths
of voyageurs who had drowned in the dangerous waters along this
section of the Ottawa.
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. A scattering of small subsistence
farming communities developed along the shores of the river to
provide manpower for the lumber camps in winter.
In 1832, following
the War of 1812, the Ottawa River gained
strategic importance when the Carillon Canal
was completed. Together with the
Rideau
Canal
, the Carillon Canal was constructed to provide an
alternate military supply route to Kingston
and Lake
Ontario
, bypassing the route along the Saint
Lawrence River
.
Several
hydroelectric dams have
been constructed on the river.
In 1950, the dam at Rapides-des-Joachims
, was built, forming Holden Lake behind it and
thereby submerging the rapids and portages at Deux Rivières.
As an economic route, its importance was eclipsed by railroad and
highways in the 20th century. It is no longer used for log driving,
however, it is still extensively used for recreational boating.
Some 20,000 pleasure boaters visit the Carillon Canal
annually.
Today,
Outaouais Herald
Emeritus at the
Canadian
Heraldic Authority is named after the river.
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  |
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-Québec operates generators 6,
7, 8, and 9 with a capacity of 89 MW.
See also
References
External links