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Lule River
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Lule River
Lule River (Lule Sami: Julevädno, Swedish: Lule älv, Luleälven) is a major river in Sweden, rising in northern Sweden and flowing southeast for 460 km (290 mi) before reaching the Gulf of Bothnia at Luleå. It is the second largest river by watershed area and length in Norrbotten County (after the Torne River and very slightly ahead of the Kalix River, which is 460.65 km long), but is the largest by average discharge.
It has a watershed of 25,240.5 km2 of which 24,545.6 km2 is in Sweden and 694.9 km2 in Norway.
The river is an important source of hydroelectric energy, with major hydroelectric plants at Porjus and the 977 MW Harsprånget, commissioned in 1952 and expanded in 1983 to become Sweden's largest hydro power station. The waterfall Harsprånget previously found at the location (former name: Njommelsaska) was the largest waterfall on the Swedish Lule River.
The river was used extensively for the transportation of timber, with logs floated downstream for processing at Luleå, but this stopped in the early 1980s.
The Greater Lule River (Big Lule River) arguably begins somewhere near Bajep Sårjåsjávrre in Norway, just east of Blåmannsisen glacier. The water flows over the border to the Virihaure lake in Padjelanta National Park, which also collects water from Kerkevare (via Kettaurejokk) and Alkajaure (via Millätno). The Tukejokk joins the Lule as well in Virihaure. Leaving Virihaure to the north, the river reaches the Vastenjaure lake after losing 32m over 2.2 km. It then flows via the Vuojatätno to lake Kutjaure and then Luoktanjarkajaure, collecting a lot of water from other lakes in Sarek National Park, like Salohaure, and from the Swedish-Norwegian border, before entering the Akkajaure reservoir, which has a storage capacity in excess of 6 km3, constituting the largest man-made lake in Sweden.
The creation and expansion of the reservoir as well as the later added power plant Vietas meant the curtailment of flow downstream to the waterfall Stora Sjöfallet, where the water falls 39.6 m from Kårtjejaure to Langasjaure and which used to be known as one of the most impressive waterfalls in Sweden. In the latter of the lakes, the Vietasajokk joins the Lule, nowadays also through the aforementioned powerplant. After Langas, the river drops 2 meters in a small section of rapids known as Jaurekaska into Stora Lulevatten, which is the largest of the lakes in the river.
The 20 km long stretch between the outlet of Stora Lulevatten and just downstream of Ligga is particularly noteworthy for its geology and topography. Whereas the topsoil along the shore for most of the course is constituted of moraine, the river banks along this particular stretch are largely constituted of exposed bedrock. In this section, the river alters considerably to rather have the characteristics of a mountain torrent than a large river, as in its natural state, it drops more than 207 meters through a nearly continuous series of rapids and waterfalls, including those at Porjus and Harsprånget in what partly was constituted of a deep, narrow gorge, sometimes over 40 meters deep. The sustained gradient for this section is around 1%, which is extremely steep for a river of the size, considering its average flow rate here reaches 270 m3/s. The sustained, concentrated drop combined with the river's high average flow rate affords the three hydroelectric power plants along the segment, namely Porjus, Harsprånget and Ligga a combined hydroelectric potential that rivals Ulla-Førre or all the power plants along the High Rhine in productivity, as this corridor alone produces an annual average of 4.2 TWh, or 30% of the production on the entire river system, including tributaries. It is believed that the river's course in pre-glacial times downstream of Stora Lulevatten went through the Råne River valley. Later, it's believed that the river broke its present more southernly course through stream capture by the present right tributary Pakkojokk along fracture zones, with the resulting increased flow rate eroding the deeply incised valley downstream of Stora Lulevatten.
Downstream of Ligga, the river drops another 87 meters over 25 km. In its natural state, this stretch was made up of several, continuous rapids, whereas today, this section is wholly made up of the Messaure reservoir, which is dammed by a 2 km long, 100 m tall rock-fill dam, the largest in Sweden, where said drop is exploited for power generation. At this segment, the main river is joined by the Muddus River from Muddus National Park.
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Lule River
Lule River (Lule Sami: Julevädno, Swedish: Lule älv, Luleälven) is a major river in Sweden, rising in northern Sweden and flowing southeast for 460 km (290 mi) before reaching the Gulf of Bothnia at Luleå. It is the second largest river by watershed area and length in Norrbotten County (after the Torne River and very slightly ahead of the Kalix River, which is 460.65 km long), but is the largest by average discharge.
It has a watershed of 25,240.5 km2 of which 24,545.6 km2 is in Sweden and 694.9 km2 in Norway.
The river is an important source of hydroelectric energy, with major hydroelectric plants at Porjus and the 977 MW Harsprånget, commissioned in 1952 and expanded in 1983 to become Sweden's largest hydro power station. The waterfall Harsprånget previously found at the location (former name: Njommelsaska) was the largest waterfall on the Swedish Lule River.
The river was used extensively for the transportation of timber, with logs floated downstream for processing at Luleå, but this stopped in the early 1980s.
The Greater Lule River (Big Lule River) arguably begins somewhere near Bajep Sårjåsjávrre in Norway, just east of Blåmannsisen glacier. The water flows over the border to the Virihaure lake in Padjelanta National Park, which also collects water from Kerkevare (via Kettaurejokk) and Alkajaure (via Millätno). The Tukejokk joins the Lule as well in Virihaure. Leaving Virihaure to the north, the river reaches the Vastenjaure lake after losing 32m over 2.2 km. It then flows via the Vuojatätno to lake Kutjaure and then Luoktanjarkajaure, collecting a lot of water from other lakes in Sarek National Park, like Salohaure, and from the Swedish-Norwegian border, before entering the Akkajaure reservoir, which has a storage capacity in excess of 6 km3, constituting the largest man-made lake in Sweden.
The creation and expansion of the reservoir as well as the later added power plant Vietas meant the curtailment of flow downstream to the waterfall Stora Sjöfallet, where the water falls 39.6 m from Kårtjejaure to Langasjaure and which used to be known as one of the most impressive waterfalls in Sweden. In the latter of the lakes, the Vietasajokk joins the Lule, nowadays also through the aforementioned powerplant. After Langas, the river drops 2 meters in a small section of rapids known as Jaurekaska into Stora Lulevatten, which is the largest of the lakes in the river.
The 20 km long stretch between the outlet of Stora Lulevatten and just downstream of Ligga is particularly noteworthy for its geology and topography. Whereas the topsoil along the shore for most of the course is constituted of moraine, the river banks along this particular stretch are largely constituted of exposed bedrock. In this section, the river alters considerably to rather have the characteristics of a mountain torrent than a large river, as in its natural state, it drops more than 207 meters through a nearly continuous series of rapids and waterfalls, including those at Porjus and Harsprånget in what partly was constituted of a deep, narrow gorge, sometimes over 40 meters deep. The sustained gradient for this section is around 1%, which is extremely steep for a river of the size, considering its average flow rate here reaches 270 m3/s. The sustained, concentrated drop combined with the river's high average flow rate affords the three hydroelectric power plants along the segment, namely Porjus, Harsprånget and Ligga a combined hydroelectric potential that rivals Ulla-Førre or all the power plants along the High Rhine in productivity, as this corridor alone produces an annual average of 4.2 TWh, or 30% of the production on the entire river system, including tributaries. It is believed that the river's course in pre-glacial times downstream of Stora Lulevatten went through the Råne River valley. Later, it's believed that the river broke its present more southernly course through stream capture by the present right tributary Pakkojokk along fracture zones, with the resulting increased flow rate eroding the deeply incised valley downstream of Stora Lulevatten.
Downstream of Ligga, the river drops another 87 meters over 25 km. In its natural state, this stretch was made up of several, continuous rapids, whereas today, this section is wholly made up of the Messaure reservoir, which is dammed by a 2 km long, 100 m tall rock-fill dam, the largest in Sweden, where said drop is exploited for power generation. At this segment, the main river is joined by the Muddus River from Muddus National Park.
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