그로스한스도르프에서 가장 멋진 20개의 호수
그로스한스도르프에서 가장 멋진 호수를 방문하고 싶나요? 호숫가의 고요한 분위기를 느끼거나 날씨가 따뜻한 날 호수에 발을 살짝 담글 수 있다면 얼마나 좋을까요? Komoot 커뮤니티가 추천한 그로스한스도르프의 주요 호수를 아래에서 살펴보고, 다음 모험 때 직접 찾아가보세요!
마지막 업데이트: 5월 20, 2026
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호수 위에 정자가 있는 나무 부두
하이라이트 (구간) • 구조물
I do not know whether the pontoon can be walked on because the gate was closed.
번역자 Google •
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Rodenbeker Quellentag - Gasthaus Quellhof, great place to stop for refreshments with beer garden
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Due to large agricultural operations and biogas plants in the vicinity, heavy oncoming traffic with very large and fast machines can be expected all day long, especially during the harvest season, and at times there will be dirty roads and confusing road junctions and field exits!
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The Rodenbek is a river that flows into the Alster in the Rodenbeker Quellental nature reserve. The idyllic Rodenbeker pond along its course is managed by the Rahlstedt sports fishing association from 1934 e.V. and is the habitat of numerous fish species, such as carp, eel and perch. kulturlotse.de/ort/rodenbeker-teich-3806401676914271620
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Cheerful birdsong accompanies you through the beautiful deciduous forest. The frogs are croaking in the pond.
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Good asphalt, little traffic
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The Rodenbeker Quellental nature reserve is an 84-hectare glacial meltwater river system in northeast Hamburg. It lies in the former edge area of the Vistula glaciation. Locally there are elevations in the form of ground moraines. The site elevation is between 15 and 20 meters above mean sea level. The site was granted protected status on January 25, 1977, originally measuring 47 hectares. On July 26, 2011, the Hamburg Senate announced an expansion by 37 hectares to 84 hectares. In the Quellental there are extensive deposits from an ice reservoir, which are now cut through by various smaller basins, small rivers. These are the Rodenbek, the Bredenbek, the Lottbek, the Mühlenbek and other small streams. All flow in an east-west direction to the Alster, a northern tributary of the Elbe. The formation of the Rodenbeker Quellental began in the Weichselian Ice Age, when the Bredenbek Glacier slowly retreated and the meltwater at the base of the glacier found its way to the Alster. The current appearance of the spring valley is also due to spring erosion. (Source: Wikipedia)
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