クラウシュヴィッツでの 周辺の簡単なハイキングとウォーキング

On the way to Drachenberg, opposite is a water lily pond.

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It's just incredibly beautiful here 😊.

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It's just incredibly beautiful here 😊.

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Unlike many other ponds in the Muskau Fold, this is a natural pond. Also known as the Fire Tower Pond, the name of the Forest Railway stop of the same name, located just 100 meters from the pond.

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The surface collapses can be reached via a small footpath off the hiking trail. But it's worth the effort. The surface collapses here are a special feature of mining in this region. Uninitiated observers often interpret the earth's surface as the result of war, because here there are depressions next to depressions, like in a bombed field. The vegetation beneath the Drachenberg ridge path is only about 50 years old. At the time of coal mining, this was a bare area where nature had reclaimed its terrain. The term surface collapse refers to mining damage caused by collapses in the underground or on the earth's surface. The damage is visible through cracks or crater-like collapse craters. They usually occur when old, unfilled tunnels and shafts in a mine collapse. In lignite mining here, the chamber fracture method was used. This involves deliberately causing the mined lignite chambers to break. This is not a case of mining damage, but rather the legacy of a particular production method.

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The information board "Fauna and Flora" gives an insight into the natural conditions in the hiking area. Next to the board there is a small seating area. From there you have a good view of the clearing opposite. Designated as land reform land in 1945, this area was used for agriculture until the 1960s. Due to the previous agricultural use, this area is mainly covered in ground cover plants such as grass, which makes it difficult for birch and pine seedlings to gain a foothold. Otherwise, the plateaus in the hiking area are dry and usually covered with pine trees. Cranberries spread in the herb layer of these plateaus. Heather and blueberries are typical in sunny areas. Moisture-loving vegetation spreads in the Giesers. Birches are common, some oaks and various shrubs, including the Fallen Oak. Bracken fern dominates the ground vegetation. When it gets really wet, Moor grass appears. Small areas of moorland can form in the subsidence zones. When there is full vegetation, the geomorphological contours are blurred. It is therefore worth taking a step to the right and left of the hiking trail. Wolves have also recently become resident, making it difficult to see any game. Wild boars can be seen digging damage along the path.

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Three Gieser mountains were hiked up to the Doppelgieser. These differ slightly in terms of the shape of the slopes. This is mainly due to the nature of the neighboring rocks, gravel and clay. However, the Doppelgieser is not only the most striking in the area of the "Drachenberge" geo-trail. It is particularly special due to its seam position. This is described on the relevant information board. It is therefore up to approx. 100 m wide and the main depression is approx. 15 m deep. Within this main depression there are two further depressions that are cut another 2 to 4 m. The southern ascent to the Drachenberg with almost 20 meters in altitude is a particular physical challenge due to its steepness.

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There is an information board here on the subject of "Gieser". Opposite there is a place to sit and a boundary stone. This marks the boundary between Krauschwitz and Weißwasser. Weißwasser was granted town rights in 1935. The stones were placed at this time and can be found in several places. Gieser are more or less elongated, damp depressions. The glacier compression caused the layers that would otherwise lie horizontally beneath the earth's surface to become steep. They thus protruded from the earth's surface. Lying flat beneath the earth's surface, the brown coal begins to weather. It oxidizes under the influence of atmospheric oxygen. Oxidation is associated with a loss of volume. This does not apply to the neighboring rocks sand and clay. The ground above the coal seam sinks. Rainwater washes fine soil material into the Gieser from the side slopes, along with leaves that are difficult to decompose. As a result, a water-retaining layer forms in the depression. The Gieser soil becomes moist, sometimes swampy or boggy. This explains the term Gieser (sometimes Jeser). It is derived from the Wendish word jezero: swamp.

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