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Inlet Structure of Muldestausee

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Inlet Structure of Muldestausee

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Inlet Structure of Muldestausee

Recommended by 79 cyclists out of 95

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Location: Muldestausee, Anhalt-Bitterfeld, Wittenberg, Saxony-Anhalt, Germany

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Top cycling routes to Inlet Structure of Muldestausee

4.7

(100)

388

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1. View of the Mulde River – Großer Goitzschesee loop from Bitterfeld

48.7km

03:03

140m

Intermediate bike ride. Good fitness required. Mostly paved surfaces. Suitable for all skill levels.

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Intermediate

4.6

(57)

214

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2. View of the Mulde River – Polder structure Löbnitz loop from Rösa

32.1km

02:04

90m

Intermediate bike ride. Good fitness required. Mostly paved surfaces. Suitable for all skill levels.

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Intermediate

4.9

(30)

102

riders

3. View of Bad Düben – View of the Mulde River loop from Rösa

50.6km

03:12

170m

Intermediate bike ride. Good fitness required. Mostly paved surfaces. Suitable for all skill levels.

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Intermediate

Tips

Schakal

November 6, 2024

The old bridge will now be renewed by 2027, according to plan 😃

Translated by Google •

Joern

July 24, 2020

a look at the inlet structure of the Muldestausee

The Muldestausee is a flooded open pit in the Anhalt-Bitterfeld / Saxony-Anhalt district. Its locations are Friedersdorf, Schlaitz, Pouch and Mühlbeck. With a surface area of 6.3 km², it is the fourth largest body of water in Saxony-Anhalt. Its length is approx. 9 km, its widest point 2 km, the greatest depth 35 m.
After the mining of the Muldenstein open-cast mine (1954–1975), the trough had to be moved over a distance of about eleven kilometers in order to expand the Goitzsche open-cast mine (today's Großer Goitzschesee). Part of the new course of the river was laid through the carburized Muldenstein open-cast mine. The flooding took place from April 30, 1975 to March 1, 1976. The Muldestausee has an inlet and an outlet structure.
The normal water level is around 79 m above sea level. NN at approx. 110 million m³ storage volume. The role of the Mulde reservoir as a flood retention basin is insignificant. However, the pool can temporarily withhold 15 million m³ at times (difference between total storage space and storage space). As a result, it is not actually a reservoir, but a river dam. As the flow velocity slows down when the trough flows in, the Mulde reservoir is a sedimentation trap into which approx. 400,000 t of solids (gravel, sand, silt) are introduced annually. The river lacks these solids when it leaves the outlet structure, which leads to a deepening of the river bed of the lower trough and has ecological effects.

de.wikipedia.org/wiki/Muldestausee

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Elevation 90 m

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Saturday 25 October

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8°C

70 %

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Max wind speed: 16.0 km/h

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Location: Muldestausee, Anhalt-Bitterfeld, Wittenberg, Saxony-Anhalt, Germany

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View of Muldestausee Near Pouch

Swimming Spot at Lake Goitzsche

View of Lake Goitzsche

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Roter Turm Pouch

Inlet Structure of Muldestausee

1. View of the Mulde River – Großer Goitzschesee loop from Bitterfeld

2. View of the Mulde River – Polder structure Löbnitz loop from Rösa

3. View of Bad Düben – View of the Mulde River loop from Rösa

Other Popular Places to Check Out

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