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15-678: Kander may refer to:is an Albanian village Rivers [ edit ] Kander (Switzerland) Kander (Germany) People with the surname [ edit ] Jason Kander (born 1981), American politician John Kander (born 1927), American composer of the songwriting team Kander and Ebb Lizzie Black Kander (1858-1941), American writer and activist Nadav Kander (born 1961), British photographer Simon Kander (1848-1931), American politician See also [ edit ] Chander Sander (disambiguation) Xander (disambiguation) Zander (disambiguation) Topics referred to by

30-566: Is a lake in the Bernese Oberland , Switzerland , 4 kilometres (2.5 mi) east of Kandersteg in the Oeschinen valley. At an elevation of 1,578 metres (5,177 ft), it has a surface area of 1.1147 square kilometres (0.4304 sq mi). Its maximum depth is 56 metres (184 ft). The lake was created by a giant landslide and is fed through a series of mountain creeks and drains underground. The water then resurfaces as

45-701: Is different from Wikidata All article disambiguation pages All disambiguation pages Kander (Switzerland) The drainage water from the Kander Neve (glacier) in the middle of the Bernese Alps at an altitude of 2,301 m (7,549 ft) flows through the Gasteretal westward. 3 kilometres (1.9 mi) south of Kandersteg it turns to north into the larger Kandertal . After 14 kilometres (8.7 mi) it converges in Frutigen with

60-486: Is possible on the ice. Fish in the lake include Arctic char ( Seesaibling ), lake trout ( Kanadische Seeforelle ), and rainbow trout ( Regenbogenforelle ). From January to March, ice fishing is popular. A gondola lift from Kandersteg leads to Oeschinen, 25 minutes by foot from the lake. Since 2007 the lake has been part of the Jungfrau - Aletsch - Bietschhorn UNESCO World Heritage Site . As of summer 2021,

75-743: The Engstlige from the left, its second major tributary. The Engstligental with Adelboden at its south end, runs more or less parallel to the Kandertal before they converge into the Frutigtal . Continuing northwards, the Frutigtal makes a long bend to the west in order to get around the Niesen . Between Spiez and Reutigen it converges with the Simme from the left, its major tributary, and turns to

90-498: The Oeschibach . Part of it is captured for electricity production and as a water supply for Kandersteg. In observations from 1931 to 1965, the elevation of the lake surface varied between 1,566.09 metres (5,138.1 ft) and 1,581.9 metres (5,190 ft). The average seasonal variation was 12.2 metres (40 ft) (September/April). The lake is generally frozen for five months, from December to May. From time to time ice skating

105-536: The city of Thun and Uttigen . As a result, the Allmend was repeatedly flooded. As the river flowed within a few hundred meters of Lake Thun , there were early proposals to divert the river into the lake, thus avoiding the Allmend and stopping the flooding. At the beginning of the 18th Century, the engineer Samuel Bodmer created plans involving a cutting through the Strättlighügel ridge that separated

120-630: The Aare in the 1870s, and a flood relief tunnel in the early 21st century. With respect to rafting , the Kander is classified as unrunnable (level VI on the International Scale of River Difficulty ) due to the river's numerous rapids and barriers. In 2008, a Swiss Army rafting party's inflatable boats capsized during an attempt to navigate the river; five soldiers were killed. Oeschinensee Oeschinen Lake (German: Oeschinensee )

135-620: The north again and flows into the Lake of Thun after a break through a hill, which used to prevent it flowing into the lake until 1714. Here the river crosses the A6 motorway . The source of the Kander is fed from the Kanderfirn glacier in the Blüemlisalp massif. Initially the river in an easterly direction, until it turns sharply north just south of the village of Kandersteg . This section of

150-624: The northern portal of the Lötschberg tunnel , which passes under the Gastertal on its way to Brig and the Rhone Valley . A road also follows the valley to Kandersteg and beyond into the Gastertal, but unlike the railway this is a dead-end, with no through road route across the mountains. The Kander originally flowed through the low lying Thun Allmend area and entered the Aare between

165-485: The river and lake. The plans were approved in 1711, and work began but was delayed by the second Battle of Villmergen . In the spring of 1713 work restarted under the direction of Bern's city architect Samuel Jenner , but with a tunnel instead of the unfinished cutting. Work was finished by the end of the year, but in 1714, the river started to enlarge the channel, causing the tunnel to collapse and creating today's Kanderschlucht or Kander canyon. The Kander correction

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180-463: The same term [REDACTED] This disambiguation page lists articles associated with the title Kander . If an internal link led you here, you may wish to change the link to point directly to the intended article. Retrieved from " https://en.wikipedia.org/w/index.php?title=Kander&oldid=1130074424 " Categories : Disambiguation pages Disambiguation pages with surname-holder lists Hidden categories: Short description

195-586: The valley is known as the Gastertal. In Kandersteg, the Öschibach , a tributary stream that drains the Oeschinensee , joins the Kander. The river then runs north through Kandergrund as far as Frutigen , where it is joined by another tributary, the Engstlige . Below Frutigen the river flows through Reichenbach im Kandertal , where it meets the Chiene , and Mülenen , where it meets the Suld . Finally, near

210-572: The village of Wimmis , it meets the Simme . The valley downstream of Frutigen is known as the Frutigtal. The last short section of today's river, the Kanderschlucht or Kander canyon, is artificial, having been created as a result of the Kander Correction (see below). At the end of the canyon, the river flows into Lake Thun . Between Mülenen and Kandersteg, the river is followed by the Lötschberg railway line on its climb to

225-485: Was the first piece of major water course re-engineering in Switzerland and lack of experience subsequently led to problems. The amount of water flowing into Lake Thun was increased by 60%, with a commensurate increase in outflow through the city of Thun. This caused flooding and bank correction, which has been addressed over the years in different ways, including channeling of the Aare in 1716, a more major correction of

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