4.6
(2069)
9,477
ハイカー
38
ハイキング
ミッテルハヴィヒスドルフ 周辺でおすすめのハイキングやウォーキングを楽しんでいただけるように、このエリアの小径やルートを集めたkomootコレクション全体を見直しました。 以下で各ルートの詳細をご覧になり、ミッテルハヴィヒスドルフ周辺の大自然を満喫する際の参考にしてください。
最終更新日: 3月 29, 2026
4.3
(7)
19
ハイカー
5.30km
01:28
90m
90m
初級者向けハイキング. あらゆるフィットネスレベルに適しています。 進みやすいルートです。あらゆるスキルレベルに適しています。
5.0
(4)
9
ハイカー
9.21km
02:35
180m
180m
中程度のハイキング. ある程度のフィットネスレベルが必要です。 進みやすいルートです。あらゆるスキルレベルに適しています。
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4.0
(3)
15
ハイカー
13.3km
03:36
180m
180m
中程度のハイキング. ある程度のフィットネスレベルが必要です。 進みやすいルートです。あらゆるスキルレベルに適しています。
4.7
(3)
12
ハイカー
8.79km
02:20
80m
90m
中程度のハイキング. ある程度のフィットネスレベルが必要です。 進みやすいルートです。あらゆるスキルレベルに適しています。
4.8
(4)
13
ハイカー
4.28km
01:07
30m
30m
初級者向けハイキング. あらゆるフィットネスレベルに適しています。 進みやすいルートです。あらゆるスキルレベルに適しています。
さらに多くのルートや他のユーザーのおすすめ情報を確認できます。
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The lake is very overgrown, making swimming a bit of a deterrent. You can easily walk around the lake and then come to a kiosk selling delicious food and drinks.
1
0
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.
1
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Learning to deal with nature, not just for children. Discovering new things and refreshing your own knowledge is possible here.
3
0
Unfortunately a part of him has been destroyed, it's a shame.
1
0
Beautiful well-kept refuge at a crossroads.
1
0
Very well-kept area with a lawn, play equipment and a former kiosk.
0
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Old bridge over the Mandau River in Mittelherwigsdorf. More information: https://de.wikipedia.org/wiki/Mittelherwigsdorf and https://de.wikipedia.org/wiki/Mandau
1
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Nice decoration on the house.
1
0
他の地域の最高のハイキングを見てみましょう。
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