Concept

Torne

Résumé
The Torne, also known as the Tornio (Tornionjoki, Torne älv, Torneälven, Duortneseatnu, Väylä), is a river in northern Sweden and Finland. For approximately half of its length, it defines the border between these two countries. In the upper parts, the river is situated in Sweden before it meets the Muonio River where it adjoins the international border. It rises at the lake Torneträsk near the border with Norway and flows generally southeast for a distance of into the Gulf of Bothnia. It is the largest river in Norrbotten County both by length and by watershed area. At its source, Torne is located close to the North Atlantic and Narvik on the other side of the watershed, with several thousands of kilometres between the locations via waterways. The Torne basin has a total area of or (see sidebar). Of this, or is in Sweden, or is in Finland and or is in Norway. The source of the Torne is generally believed to be the lake Torneträsk near the border with Norway. But the main feeder of this lake is Abiskojåkka, flowing out of Abiskojaure, which is mainly fed by Kamajåkka, coming from tributary Gamajávri. This lake's major tributary is Válfojohka. That river comes from Lake Válfojávri in Norway's Nordland, but near to that lake it is joined by a nameless, longer stream, according to official Swedish maps fed by a small glacier, above sea level (). Other affluents of Lake Torne are Njuoraätno and Kåppasjåkka in the west, Gurttejohka, Snurrijåkka, Bessešjohka, Bággesgorsajohka, Davip Duoptejohka, Lulip Duoptejohka, Sarvájohka and others in the north, and Rákkasjohka, Gohpasjohka, Miellejohka, Bessešjohka, Golkkokjohka, Nivsakkjohka and others in the south. Above Torne lake, the watershed of the Torne includes the villages Riksgränsen, Katterjåkk, Vassijaure, Låktatjåkka, Kopperåsen and Tornehamn. On the south shore of Torne lake are Björkliden, Abisko, Stordalen, Kaisepakte. Stenbacken and Torneträsk. On the north shore are the Sami villages Laimoluokta and Kattuvuoma.
À propos de ce résultat
Cette page est générée automatiquement et peut contenir des informations qui ne sont pas correctes, complètes, à jour ou pertinentes par rapport à votre recherche. Il en va de même pour toutes les autres pages de ce site. Veillez à vérifier les informations auprès des sources officielles de l'EPFL.