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Kangiqsualujjuaq (/ k æ n ˌ dʒ ɪ k s u ˈ æ l uː dʒ u æ k /; French: [kɑ̃dʒiksɥalydʒɥak]) [4] is an Inuit village located at the mouth of the George River on the east coast of Ungava Bay in Nunavik, Quebec, Canada. Its population was 956 as of the 2021 census.
Paradise River is a community on the southwestern coastline of Sandwich Bay in southeastern Labrador, Canada.. Located at the outlet of the river for which the community is named, it is situated along Route 516, the Cartwright Highway, which connects Paradise River to the town of Cartwright as well as the Trans-Labrador Highway (Route 510), which in turn is connected to Happy Valley-Goose Bay ...
The Canadian Heritage Rivers System (CHRS; French: Le réseau de rivières du patrimoine canadien) is a joint program administered by the federal, provincial, and territorial governments to conserve and protect the best examples of Canada's river heritage, to give them national recognition, and to encourage the public to enjoy and appreciate them. [1]
The Lakes to Locks Passage in the United States and the corresponding Route du Richelieu in Canada form a scenic byway network located in northeastern New York and southern Quebec. This byway connects a series of water routes including the upper Hudson River, Champlain Canal, Lake George, and Lake Champlain. This network is part of a ...
At Nosamwokwu Lake, [7] the river turns east and meets the Saskatchewan River at The Pas, just downstream from Carrot River. [8] [9] In 1941, the Pasquia River Control Structure (Knapp Dam) [10] was built by Ducks Unlimited Canada to control the waters from Pasquia Lake and improve conditions for waterfoul. Big Lake (which naturally drains into ...
The Harrison River is a short but large tributary of the Fraser River, entering it near the community of Chehalis, British Columbia, Canada. The Harrison drains Harrison Lake and is the de facto continuation of the Lillooet River , which feeds the lake.
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The Canard River has a short length of 15 km but its lower reaches are wide and deep due to the enormous tides of the Minas Basin. The river was once tidal for most of its length but a series of dykes first built in the 1600s held back the tide which is now stopped near the river's mouth by the Wellington Dyke. The upper reaches of the river ...