훔멜탈 주변 최고의 협곡은 프랑켄슈바이에른의 가장자리에 위치한 다양한 풍경을 특징으로 하는 지역에서 찾을 수 있습니다. 이 지역은 탐험에 적합한 암석 지형과 계곡을 포함한 다양한 자연 명소를 제공합니다. 물에 의해 형성된 풍경은 협곡과 깊은 계곡과 유사한 특징을 만들어냅니다. 방문객들은 자연 및 지질학적 하이라이트가 혼합된 다양한 하이킹 트레일을 통해 자연의 아름다움을 발견할 수 있습니다.
마지막 업데이트: 4월 12, 2026
번역자 Google •
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하이라이트 • 협곡
번역자 Google •
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하이라이트 • 자연 기념물
번역자 Google •
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It's beautiful how the clear water rushes over the mossy rocks. It's not one of the big waterfalls, but it's enchanting nonetheless.
15
4
One rock more interesting than the other, a highlight in Saxon Switzerland.
16
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Between the narrow rock walls and the single trail make the path particularly nice to explore.
15
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The blocks of different sizes consist mostly of silicified sand. Most of the natural monument is located just a few meters south of the border between Germany and Belgium in the area of the Belgian municipality of Raeren and is divided by the Aachen Landgraben. However, some of the Cyclops stones can be found on German soil.[2] The starting material for the formation of the Cyclops stones was unconsolidated Upper Cretaceous sand, the so-called Aachen sand, which is widespread in the Aachen Forest area and used to be found in numerous sand pits, e.g. B. the Flög sand pit in Hauset was mined. The Aachen sand was deposited in the Santonian in the area of a shallow sea 85 to 84 million years ago. The tropical climatic conditions during the Upper Cretaceous and Tertiary led to a near-surface solution of quartz from the Cretaceous sands through the penetration of precipitation water. In deeper soil layers, the siliceous solutions were precipitated again under special chemical environmental conditions and then led to partial silicification of the sand deposits.[3] Such formations are called Tertiary quartzites and are quite widespread at high altitudes in the European low mountain ranges. The unconsolidated areas of the Aachen sands have been removed by erosion, so that the cyclops stones now lie on the surface as relics. Previous theories of origin assumed that the Cyclops stones were originally in a higher morphological position. During the Ice Age, the stones are said to have slipped to their current position.[4] This theory is now considered refuted. Source: Wikipedia
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Unfortunately it was dry when we visited, so it's best to visit after the snow has melted or there has been heavy rain.
5
4
Nice path through and past the dolomite rocks.
4
2
This rock path is marked several times as a highlight. Thanks to GPS corruption, high frequency and much more.
4
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