The best cycling routes around Muldestausee

This view from the circular path onto the Goitzsche is always beautiful again.

Simply wonderful 👍

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)

The village of Seelhausen was buried in 1987 during the expansion of the Goitzsche open-cast mine. The Seelhausen Lake was created by flooding the remaining open-cast mine pit. It lies west of Löbnitz, south of Bitterfeld, and north of Delitzsch, in the Central German Lake District. From the end of July 2000, the lake was filled with water from the Mulde River via a pipeline at a rate of 1 m³/s[1] until the pipeline was destroyed by the Elbe River flood in 2002. Since then, the lake has been fed by the Lober-Leine Canal. According to the LMBV (Lausitz and Central German Mining Company), 96% of the planned water level had been reached by March 2004. The flooding work was completed in 2005.[1] A beach area has since been built at the flooding site, and further development of the lake as a recreational area is planned. The larger Goitzsche Lake lies northwest of the Seelhausen Lake. The lake district also includes Lake Paupitzsch, Lake Holzweißig, Lake Ludwig, Lake Neuhaus, and Lake Zöckeritz with Essigloch and Lake Auensee. The total surface area of all lakes in the former Goitzsche open-cast mine is estimated at 24 square kilometers. Lake Seelhausen is a former open-cast mine lake with a water level of 78 meters above sea level. Its storage capacity is 74 million cubic meters, with a surface area of 622 hectares. Source: https://de.wikipedia.org/wiki/Seelhausener_See

Lake Seelhausen is a former open-cast mining lake of approximately 622 hectares, formed from the former Rösa lignite mine (part of the Goitzsche). It lies mostly in the German state of Saxony and partly in Saxony-Anhalt. Source: https://de.wikipedia.org/wiki/Seelhausener_See

The outlet structure of the Löbnitz polder (Nordsachsen district) was completed today (May 12, 2022). It is an important component of the controlled polder system and is located north of Löbnitz. The structure consists of a 300-meter-long fixed overflow weir and five movable gates, known as sluices, with a total opening width of 40 meters. Normally, the sluices are closed. When the polder is flooded, the gates are only opened after the water level between the polder and the Vereinigte Mulde river has been measured. Construction of this structure began in February 2020 and cost approximately six million euros, financed by the National Flood Protection Program. Background information: During the August 2002 floods, the Vereinigte Mulde river experienced severe flooding. This revealed that the existing flood control structures near the river were causing high flow velocities and discharge depths. The dikes were overtopped and breached in several places. The Löbnitz polder now provides the Vereinigte Mulde river with the necessary floodplains. Construction of the polder has been underway since 2011. The controlled flood protection system covers an area of approximately 1,400 hectares and can hold around 15 million cubic meters of water. Floodwaters can also be channeled through the polder to reduce the flow velocity and thus prevent dike breaches and erosion. For this purpose, the existing dikes are being repaired to their current level of protection and will form the future polder dike. In the event of a major flood, the water will be channeled through the polder via reinforced inlet and outlet structures. Further information about the Löbnitz polder can be found on the following website: www.polder-loebnitz.de. Floodwater runoff can also be directed through the polder to reduce the flow velocity and thus prevent dike breaches and erosion. Source: https://www.medienservice.sachsen.de/medien/news/1044944 Source https://loebnitz-am-see.de/buerger-gemeinde/brand-und-katastrophenschutz/deichanlage-polder/

Construction of the new bridge began in 2025 and it will run parallel to the old bridge.

Great view