마지막 업데이트: 3월 3, 2026
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하이라이트 • 기념물
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하이라이트 (구간) • 트레일
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The Mulde, also known as the United Mulde or Vereinte Mulde, is a left, non-navigable tributary of the Elbe. It originates southeast of Leipzig near Sermuth (Saxony) from the confluence of two large headstreams: the longer Zwickauer Mulde and the Freiberger Mulde, which drains a larger catchment area due to its greater discharge. The river's catchment area encompasses large parts of Saxony and, in particular, the vast majority of the northern slopes of the Ore Mountains. With a discharge of approximately 73 m³/s at its mouth,[8] it is the fourth largest tributary of the Elbe. The old name for the Mulde, Milda, is translated by onomasticians as "the water-rich one."[9] The word element "Mel," referring to grinding, is sometimes associated with the name due to the numerous mills that once operated along the river. This overlooks the fact that river names represent the oldest, often Slavic or Celtic, layer of geographical names. The Mulde's name is sometimes linked to the numerous mills that once operated along its banks, but this connection overlooks the fact that river names represent the oldest, often Slavic or Celtic, layer of geographical names. Source https://de.wikipedia.org/wiki/Mulde_(Fluss)
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Many types of water sports are possible, including sailing, surfing, camping, hiking, fishing, etc. The lake has very good water quality and a large number of fish. There is a nature trail between the towns of Pouch and Friedersdorf. Until the end of 2009[3][4][5] there was a passenger ship ("Muldeperle") on the lake that made round trips. The ship was taken over by the transport company Vetter Verkehrsbetriebe.[6] On the north bank of the Mulde Reservoir there is the Haus am See, an information center for the environment and nature conservation with a permanent exhibition on the history and development of the lake. The Mulde Reservoir is part of the Central German Lake District and is located on the coal-steam-light cycle path that leads from Wittenberg to the Leipzig Neuseenland.[7] Source https://de.wikipedia.org/wiki/Muldestausee
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The dam near Friedersdorf is a 19 m high and 303 m long gravity dam with a structure volume of 40,000 m³. On February 17, 2023, a hydroelectric power plant was put into operation that is expected to generate 13.6 GWh of electrical energy per year. Construction cost 25 million euros and began in October 2016.[1][2] Source https://de.wikipedia.org/wiki/Muldestausee
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The normal water level is around 79 m above sea level with a storage volume of around 115 million m³. The role of the Mulde reservoir as a flood retention basin is insignificant. However, the basin can temporarily hold back 3 million m³ during floods (difference between total storage capacity and storage capacity). As a result, it is not a reservoir in the true sense of the word, but a river dam. Since the flow rate of the Mulde slows down considerably when it flows in, the Mulde reservoir is a sedimentation trap into which around 400,000 tonnes of solids (gravel, sand, silt) are carried every year. These solids are missing from the river when it leaves the outlet structure, which leads to a greater deepening of the riverbed of the lower Mulde and has ecological effects. Source https://de.wikipedia.org/wiki/Muldestausee
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After the Muldenstein opencast mine had been mined out (1954–1975), the Mulde had to be relocated over a distance of around eleven kilometers in order to expand the Goitzsche opencast mine (today's Großer Goitzschesee). Part of the new river course was laid through the mined Muldenstein opencast mine. The flooding took place between April 30, 1975 and March 1, 1976. The Mulde reservoir has an inlet and an outlet structure. Source https://de.wikipedia.org/wiki/Muldestausee
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The Muldestausee is a flooded open-cast mine in the district of Anhalt-Bitterfeld/Saxony-Anhalt. Its neighboring towns are Friedersdorf, Schlaitz, Pouch and Mühlbeck. With a surface area of 6.3 km², it is the third largest body of water in the state of Saxony-Anhalt. It is around 9 km long, 2 km wide at its widest point and 35 m deep. Source https://de.wikipedia.org/wiki/Muldestausee
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It's now almost impossible to recognize it as a path. Everything is overgrown!
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