Река Мадавоска: История, География и Экология

the Madawaska River in Quebec/New Brunswick

The Madawaska River flows from Lake Témiscouata in Quebec, through Degelis, Quebec, to join the Saint John River at Edmundston, New Brunswick. The course of the Madawaska River is accessible in Quebec by route 185 and New Brunswick by Highway 2, which run along the river side South West.

Various theories exist over the etymology of the word Madawaska. One is that the river's name comes from the Algonquian word "Madoueskak", which means "land of the porcupine". In Maliseet, the word "Matawaskiyak" translates to "at the place where water flows out over grass", there is also speculation that it refers to the 'meeting of two rivers where there is grass'. The Madawaska river is a large drainage basin for Lake Temiscouata and other waterways from the north. Before the city of Edmundston changed the natural course of the river, the spring freshet would cause several branches of the river to flood the land resulting in various waterfalls. The river formed part of the Témiscouata Portage, a canoe and land route from the Bay of Fundy to the Saint Lawrence River dating from the late 17th century. A road, now Route 185 and part of the Trans Canada Highway, was built along this route in 1862. The Témiscouata Railway was built along the same route in 1886. In the early 20th century, timber and logs were floated down the river to New Brunswick. The Petit Témis Interprovincial Linear Park is a rail trail running from Edmundston, NB to Cabano, QC in the abandoned CN rail corridor that was originally built by the Temiscouata Railway. The toponym "Madawaska River" was officialized as of December 8, 1968, at Commission de toponymie du Québec (Quebec Geographical Names Board).

The river actually begins its course at the foot of the dam Lake Temiscouata. The dam, built in 1930 by the "St. John River Storage Company", was acquired by Hydro Québec during nationalization of electricity in 1963. It was completely rebuilt between 1993 and 1994. The construction of this dam has had the effect of raising the lake level of about sixty centimeters above the normal high water level, set at , to reach the level of The dam allows for storing of additional water from Lake Témiscouata, less than 6% of the volume of water contained naturally in the lake. Another consequence of the enhancement of Lake Témiscouata is the relative youth of the shores which limits the number of natural beaches and potential for recreation.