가장 멋진 협곡 6곳

A very beautiful stream valley. The path sometimes leads directly along the stream and then again a few meters away. There is a wonderful deciduous forest on the eastern slope in particular, which creates a wonderful backdrop with its fresh green in spring.

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The Roschertal owes its existence to a geological peculiarity. It is a breakthrough valley of the Mandau, which has cut through a basalt layer and underlying tertiary tuff layers. Such valleys are formed when a river erodes rock over long periods of time, while the surrounding area may rise or the water cuts deeper. Geological development: 1. Tertiary deposits: In the Tertiary period (around 65 to 2.6 million years ago) the area was characterized by volcanic activity. Tuff - a rock made of volcanic ash - was deposited. Later, basalt flows poured over it and formed a resistant covering layer. 2. Cutting of the Mandau: The Mandau, a tributary of the Neisse, began to work its way through the harder basalt layer over time. Since basalt is much more resistant than the tuff underneath, the erosion process was uneven. The softer rock layers were eroded more quickly, so that the valley gradually deepened. 3. Formation of the breakthrough valley: As the rock was further eroded, the steep, wooded slopes of the Roschertal that are visible today were created. These reach heights of around 50 to 60 meters above the valley floor. 4. Late Pleistocene influence: During the ice ages, the landscape was further shaped when frost weathering and landslides affected the valley flanks. During this time, the Mandau transported more meltwater and debris, which caused the river to dig in further. Special features today: The Roschertal is not only a geologically interesting area, but also an example of the natural development of Upper Lusatia. The interplay of basalt and tuff layers gives the landscape a varied morphology. Erosion has created some bizarre rock formations, and the forest that has developed in the valley protects the loose rock layers from further erosion. The fact that the Mandau has formed a breakthrough valley here also influences the water dynamics. The flow can vary greatly depending on the water level, which is noticeable in small cascades and whirlpools. In summary, the Roschertal is a product of the volcanic past, fluvial erosion and ice age processes - an exciting geological formation that also offers an attractive landscape for hikers and nature lovers.

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A real insider tip for a nice hike without many people.

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There is a gas station just after the bridge on the Polish side.

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The Georgewitzer Skala was created over a length of approx. 1.3 km by the erosive action of the Löbau water as a deeply incised, south-north oriented, canyon-like rocky valley (skala = Slavic term for rock). This form of a breakthrough valley is more common in Upper Lusatia, especially in the Upper Lusatia region (cf. Gröditzer scale, Lausk scale). The geological source rock, the West Lusatian granodiorite or the Zweiglimmergranodiorite, was removed by the erosion process over thousands of years. The geological subsoil is mainly covered by nutrient-rich loess loam and river gravel from the Vistula ice age. The valley has steep slopes, rock faces and crevices, the Löbau water has a near-natural stream bed with many blocks. The wooded rocky slopes on both sides of the stream rise from 210 m above sea level. NN in the valley floor up to a height of 240 m above sea level. NN and go with a moderate incline into a plateau. A large number of very different near-natural forest communities, such as pedunculate oak-hornbeam forest rich in linden trees, sessile oak-beech forest rich in hornbeam and hornwort-black alder shoreline characterize the scale. As special features of the avifauna, kingfishers, lesser woodpeckers and gray wagtails can be mentioned. Hollow Corydalis, Black Lungwort, Lily of the Valley and Greater Chickweed occur as protected plant species due to the weakly alkaline-influenced granodiorite weathering soil of the basalt mountains. Source: Wikipedia

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The Kemmlitz is a seven-kilometer-long stream that flows through the villages of Burkersdorf, Schlegel and Hirschfelde. It rises on the western slope of the Buchberg in the Oberwald, later flows through several ponds in Schlegel and unites with the Dittelsdorfer Wasser in the Kemmlitztal. About a kilometer further on, the Kemmlitz flows into the Lausitzer Neisse near Rosenthal. The section marked here begins around the Schlegeler Mühle and leads to the B99, at the entrance to Hirschfelde. Is primarily a hiking trail, but can also be used with a normal touring bike or MTB.

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Grottau Bridge, crossing into a small piece of Poland or further to the Czech Republic

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Great gorge in a small space.

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The bridge is finally open again.

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This path does not lead directly along the Kemnitzbach, but is particularly beautiful in my view due to its location on the edge of the forest. There are also a number of benches for a rest.

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The breakthrough valley washed out by the slowly flowing Löbauer water is a protected area. You walk through a unique area with beautiful beech, linden and oak forests, in which plants and animals worth protecting, such as the kingfisher and swallowtail, are to be found.

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The bridge is the connecting link to our neighbors Poland and Czech. On the left and right side of the Neisse you can walk towards the border triangle b.z.w. drive.

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For now the first bridge that leads from the German side over the Neisse. As an automobile bridge, she will remain number 1. The shores of the Neisse still connected until 2013, the sky bridge, which was located 200 meters from the three countries downstream point downstream, but was demolished due to their poor technical condition. The cities of Hrádek nad Nisou, Zittau and Bogatynia are currently working to build a circular bridge directly above the confluence of both watercourses.

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