데사우-로슬라우 최고의 라이딩 경로

멋진 정원 왕국, 언제나 들를 가치가 있습니다.

뮬데 댐이 보이는 다리에서 멋진 전망

꼭 볼 가치가 있습니다

꼭 볼 가치가 있습니다

데사우 시청 광장(Dessauer Rathausplatz)은 데사우-로슬라우 시의 중심지이며 도시의 랜드마크로 여겨지는 데사우 시청이 있습니다. 시청의 역사는 1336년 알브레히트와 발데마르 공작이 양도했을 때로 거슬러 올라갑니다. 시청은 1882/83년에 이루어진 확장과 1901년에 지어진 축제 공간을 포함하여 여러 차례의 중요한 개조와 확장을 거쳤습니다. 수많은 증축과 개조에도 불구하고 공간이 더 이상 충분하지 않아 1899년에 신축 건물 착공이 시작되었습니다. 신축 건물은 1901년에 완공되었으며 아르누보 건축의 예입니다.

It's about time everything turned green again 😊

The Mulde River flows entirely within the North German Plain, initially through the Saxon Hills and past Grimma, Nerchau, and Trebsen. Near Wurzen, along whose western edge it runs, the Mulde reaches the Elbe-Mulde Lowland. It then flows through Eilenburg and Bad Düben and shortly thereafter leaves Saxony. The Mulde completes the remaining course of its journey to its confluence with the Elbe in Saxony-Anhalt. Until 1975, the Mulde flowed west of the towns of Pouch and Friedersdorf in the area of what is now Lake Goitzsche. Since then, it has been dammed east of these towns to form the Mulde Reservoir – a former open-cast mine. The Mulde then flows past Muldenstein, Jeßnitz, Raguhn, and Dessau, emptying into the Elbe between Dessau and Roßlau after a course of 147 km.[2] [2] The "Wild Mulde" revitalization project for the lower reaches of the Mulde 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)

Although the confluence of the two source streams occurs at approximately half the total length of the Mulde River, the Freiberger Mulde and the Zwickauer Mulde already contribute over 80% of its total water volume. This is due, firstly, to the shape of the catchment area, which is very wide in the Ore Mountains and narrows towards the Elbe River, and secondly, to the higher precipitation and correspondingly higher runoff volumes in the mountains. The shape of the catchment areas also means that the longer Zwickauer Mulde is the smaller of the two source streams at the confluence. The Zschopau is the dominant hydrological branch of the Freiberger Mulde river system. In its upper catchment area, the Flöha, a named tributary, contributes the largest volume of water and is thus the actual source stream of the Mulde. The Mulde is approximately 267 kilometers long via this main route and over 314 kilometers via its longest route (the Zwickauer Mulde).[3] [3] The Mulde's catchment area has a total gradient of 600 to 900 meters for many of its major channels, resulting in exceptionally high flow velocities for northern Germany. The Mulde is sometimes even described as the fastest-flowing river in Central Europe.[10] Source: https://de.wikipedia.org/wiki/Mulde_(Fluss)