Rivière Saint-Maurice, 563 km long, rises upstream from Réservoir Gouin, 200 km west of Lac Saint-Jean, Québec. It drains a basin of 43 300 km2. After its confluence with Rivière Manouane, it feeds Réservoir Blanc and then takes in the Vermillon, Trenche, Croche, Mattawin and Mékinac rivers.
The Fraser River is the longest river in British Columbia, stretching 1,375 km. It begins on the western side of the Rocky Mountains at Mount Robson Provincial Park, and ends in the Strait of Georgia at Vancouver. Named for explorer Simon Fraser, the river was a transportation route and source of food for the Indigenous people of the region long before Fraser travelled its waters. In 1858, gold was discovered on sandbars south of Yale, setting off the Fraser River Gold rush.2
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.
The Saskatchewan River is 1,939 km long from the Rocky Mountains headwaters to Cedar Lake in central Manitoba. When including its longest tributary, the South Saskatchewan River, the Saskatchewan River is the fourth-longest river in Canada. It’s a major tributary to the Nelson River, ultimately draining into Hudson Bay. Its name is derived from the Cree word kisiskâciwanisîpiy meaning swift-flowing river. The Saskatchewan River was a major transportation route for First Nations for thousands of years and was an instrumental transportation and resource corridor during the fur trade and early European exploration.
The North Saskatchewan River (1,287 km long, the first 48.5 km of which is designated as a Canadian Heritage River) is a major tributary to the Saskatchewan River, which ultimately flows into Hudson Bay. The mean annual flow is 241 m3/s; however, flow varies between the peak in July and minimum in February. It served as a major transportation route from the end of the last Ice Age through the mid-20th century.