캄메레이숲 주변 최고의 그래블 라이딩 코스

Magnificent view of the Mulde from the bridge

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Wide bike path through the forest and terrain. Roots repeatedly lift the asphalt, so caution is advised...

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Bitterfeld Arch

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The floating observation tower is quite an attraction and not everyone dares to go up there.

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the good old hollow

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A beautiful photo opportunity. Sometimes decorated as a candle during the Christmas season. Across the street on the shore are bars and restaurants and a playground. It's quite busy in good weather.

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Information at https://www.thallwitz.de/thallwitz_schloss.htm

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In 1968, the nave received a new roof. Gutters and lightning protection were also replaced, and a new cross was attached to the roof. Renovation of the nave began in 1971, during which a new altar was built and fitted with a new cross. This was followed in the spring of 1972 by the reinstallation of the organ and the replastering of the exterior of the nave. The ceremonial rededication of the technically overhauled organ took place in August 1992. In September 1998, the church tower was renovated, and the crowning of the tower was completed on January 23, 1999. Since the fall of 2000, visitors have been able to climb to the tower's observation deck and enjoy the panoramic view. Source: https://de.wikipedia.org/wiki/Kirche_Thallwitz

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The church was built in the 15th century, and the foundations and substructure of the church tower date from this period. Bishop Johann VI of Saalhausen commissioned the expansion of the choir and the elevation of the church tower. The latter's cap above the octagonal upper section was created in the 17th century. The inscription on the weather vane indicates the 1626 rebuilding of the nave, which likely incorporated older masonry. The ceiling received a shallow barrel vault. In 1896, extensive reconstruction took place according to plans by the architect Oswald Haenel from Dresden. The exterior of the church and church tower were completely replastered, and the church and tower roofs were re-roofed, repaired, and secured with lightning rods. Inside, the second gallery was removed in 1896, and the remaining gallery was replaced with double tiers of seating. The organ platform was widened. The windows were fitted with stained-glass cathedrals, and new vestments made of green, red, and black cloth with gold embroidery were purchased. Following the restoration, the rededication was celebrated after the Feast of the Dead, the old church consecration festival of Thallwitz, with the participation of the patron saint, the church inspectorate, and numerous pastors from the region. Source: https://de.wikipedia.org/wiki/Kirche_Thallwitz

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Very nice view

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The inn organizes a festival every year on May 1st.

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The staircase construction is also impressive. Don't be fooled, it's a double whammy. I only noticed it when I came down, and my head was confused for a moment. 🤣

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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)

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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)

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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)

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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)

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Although the confluence of the two source rivers occurs approximately halfway along the Mulde's entire course, the Freiberg and Zwickau Mulde already contribute over 80% of the total water volume. This is due, on the one hand, to the shape of the catchment area, which is very wide in the Ore Mountains and narrows towards the Elbe, and, on the other hand, to the higher precipitation and, at the same time, higher proportions of runoff water in the mountains. The shape of the catchment areas also means that the longer Zwickau Mulde is the smaller of the source rivers at the confluence. The dominant hydrological main branch of the Freiberg Mulde's river system is the Zschopau. In its upper catchment area, it is a named tributary, the Flöha, which contributes the larger water flow and is thus the Mulde's actual source river. Along this main flow path, the Mulde is approximately 267 kilometers long, and along its longest flow path (the Zwickau Mulde), a good 314 kilometers.[3] The Mulde catchment area has total gradients of 600 to 900 meters for many important flow paths, 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)

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Very nice view of the Mulde

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Great view, invites you to take photos🤣

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The Mulde, also known as the United Mulde or Vereinigte Mulde, is a left, non-navigable tributary of the Elbe. It is formed southeast of Leipzig near Sermuth (Saxony) by the union of two large source rivers, the longer Zwickauer Mulde and the Freiberger Mulde, which has a larger discharge and drains a larger catchment area. The river's catchment area covers large parts of Saxony and in particular the vast majority of the northern slopes of the Ore Mountains. With a water flow of almost 73 m³/s at the mouth[8], it is the fourth largest tributary of the Elbe. The old form of the Mulde's name, Milda, is translated by name researchers as the water-rich one.[9] The word component Mel, with reference to grinding, is sometimes associated with the name in view of the large number of mills that used to operate 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)

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