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Skeena River
Skeena River, 580 km long, rises in the northern interior of BC and flows generally SW, draining about 54 000 km2, to meet the Pacific Ocean at Chatham Sound south of Prince Rupert.
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Skeena River, 580 km long, rises in the northern interior of BC and flows generally SW, draining about 54 000 km2, to meet the Pacific Ocean at Chatham Sound south of Prince Rupert.
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Slave River, 415 km long with an estimated mean annual flow rate in excess of 4000 cubic metres per second, connects the PEACE RIVER and the drainage from lakes CLAIRE and ATHABASCA to GREAT SLAVE LAKE, forming the short upper reaches of the Slave- MACKENZIE RIVER system in the Northwest Territories. It has a sinuous, often multichannelled, course traversing the flat, extensively glaciated Archean granitic terrain of the Canadian SHIELD and is currently used almost...
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The Soper River winds southwards 108 km through the tundra-covered hills of southern Baffin Island before emptying into Soper Lake, a brackish water body, and then directly into Hudson Strait near the community of Kimmirut, Nunavut.
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Souris River, about 720 km long, rises in the Yellow Grass marshes N of Weyburn, Sask, flows SE past Estevan and wanders S across the N Dakota border before entering Manitoba.
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South Nahanni River, 563 km long, flows southeast out of the Ragged Range of the Selwyn Mountains, cuts across successive spines of the Mackenzie Mountains and empties into the Liard River.
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The South Saskatchewan River (1,392 km long) is a heavily utilized water source in southern Alberta and Saskatchewan and is a major tributary to the Saskatchewan River, ultimately discharging to Hudson Bay. Mean flow is 280 m3/s, but varies throughout the year, largely controlled by several dams and reservoirs along the river system. The South Saskatchewan River flows through an agriculturally productive region and is prone to periodic droughts and floods.
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St Clair River, 64 km long, flows in a southerly direction, connecting Lake HURON in the N with Lake ST CLAIR in the S, and forms the international boundary between Canada and the US. Its northern portion has an average width of 0.8 km and depth of 8-18 m.
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St Croix River, 121 km long, rises in the Chiputneticook Lakes and flows SE to Passamaquoddy Bay, forming part of the border between NB and Maine. It was discovered (1604) by the French, and de MONTS built the first settlement in Acadia on Ile Sainte-Croix (now St Croix I) near the river's mouth.
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The St. Lawrence River is a grand river and estuary, which together with the Great Lakes forms a hydrographic system that penetrates 3,058 km into North America. The river proper, about 1,197 km long, issues from Lake Ontario, flows northeast past Montreal and Quebec City to the Gulf of St. Lawrence. The route of early explorers and the main axis of New France, the St. Lawrence River figured prominently in Canada's early history, and it remains the focus of settlement for much of the province of Quebec. It is still the most important commercial waterway in Canada, as well as a source of electric power and natural beauty. (See also St Lawrence Lowland.)
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The St Lawrence Seaway (Great Lakes Waterway) is the system of locks, canals and channels linking the Great Lakes and the St Lawrence River with the Atlantic Ocean.
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St Marys River, one of the largest rivers in Nova Scotia, flows into the Atlantic Ocean at a point 190 km E of Halifax.
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The obvious strategic value of the river was well known to the Indigenous people before Étienne Brûlé travelled the river in 1622. Samuel de Champlain included the falls on his 1632 map.
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The Stikine River, 539 km long, rises in the Spatsizi Wilderness Park in northwestern British Columbia and flows in a wide arc north and west out of the Stikine Plateau uplands, then south through the spectacular Coast Mountains range to meet the Pacific Ocean near Wrangell, Alaska.
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The Thames River begins in a swampy area of southwestern Ontario and meanders quietly for 273 km past the cities of Woodstock, London and Chatham-Kent to empty into Lake St. Clair.
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The following article is an editorial written by The Canadian Encyclopedia staff. Editorials are not usually updated. When the first sod was turned near Cornwall, Ont., August 10, 1954, it was not so much the beginning of the great St Lawrence Seaway as a continuation of centuries of dreams.
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