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Very beautiful old church

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During the once-in-a-century flood of 2002, the Mulde river basin, along with those of the Elbe, Müglitz, and Weißeritz, was the most severely affected. During the flood of June 2013, a dam on the Mulde River leading to Seelhausener See had to be demolished to relieve the lake.[14] Source: https://de.wikipedia.org/wiki/Mulde_(Fluss)

At the end of the Elster Glaciation, the Mulde River flowed northwest from Großbothen and Großbardau through what is now the city of Leipzig, where the Saale River also temporarily flowed into it. In the process, it eroded several channels, which it refilled until the Saale Glaciation – the Markkleeberg Mulde, the Espenhain Channel, and the Leipzig Mulde, the Naunhof Channel.[13] Approximately 130,000 to 160,000 years ago, at the end of the Saale Glaciation, the Mulde River broke through near Grimma and flowed northward along its present-day riverbed. Since then, the Parthe River has flowed through the remaining Leipzig Mulde valley. Source: https://de.wikipedia.org/wiki/Mulde_(Fluss)

The Mulde River runs exclusively in the North German Plain, initially flowing through the Saxon Hills and passing Grimma, Nerchau, and Trebsen. Approximately near Wurzen, along the western edge of which it runs, the Mulde reaches the Elbe-Mulde Lowland. It then flows through Eilenburg and Bad Düben, and shortly thereafter leaves Saxon territory. The Mulde covers the rest of its course to its mouth in Saxony-Anhalt. The Mulde continued to flow west of the two towns of Pouch and Friedersdorf in the area of today's Goitzschesee until 1975. Since then, it has been dammed east of the two towns in the Mulde Reservoir – a former open-cast mine. The Mulde then flows past Muldenstein, Jeßnitz, Raguhn, and Dessau, and flows into the Elbe between Dessau and Roßlau after a distance of 147 km.[2] The "Wilde Mulde" revitalization project for the lower reaches of the river in Dessau was recognized as an official project of the UN Decade on Biodiversity in November 2018.[11][12] Source: https://de.wikipedia.org/wiki/Mulde_(Fluss)

The Mulde, also known as the United Mulde or Vereinigte Mulde, is a left-hand, non-navigable tributary of the Elbe. It originates southeast of Leipzig near Sermuth (Saxony) through the confluence of two large source rivers: the longer Zwickau Mulde and the Freiberg Mulde, which has a larger discharge and drains a larger catchment area. 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 water flow of approximately 73 m³/s at its mouth,[8] it is the fourth largest tributary of the Elbe. The old form of the Mulde's name, Milda, is translated by onomastics as "the watery one."[9] The word component "Mel," referring to milling, is sometimes associated with the name due to the large number of mills that once operated on the river, which ignores the fact that river names represent the oldest, often Slavic or Celtic, geographical name layer. Source https://de.wikipedia.org/wiki/Mulde_(Fluss)