되플링 최고의 워킹 & 하이킹 경로

이 벤치는 더 이상 존재하지 않습니다. 현재 마을 소식에 대한 정보 게시판 (꽤 관리하기 쉬움 🤭)

이 쉼터는 더 이상 존재하지 않습니다

Magnificent view over the fields and the steep edge of the Dithmarschen Altmoräne, which was formed in the last ice age.

Nice bench from which you can look at the paddocks and paths.

a very well-kept place with a covered break opportunity. The unusual construction, which consists of four huge wooden poles on which a grass-covered roof rests, is modeled on a former harvest storage facility. This construction was called "Four Rod Mountains". The roof was movable in the original. Mayor Volker Lorenzen told me that if you want to spend the night here, you should first obtain the consent of the municipality of Dörpling.

During the last ice age the glacier front of the Nordic Inland ice, coming from the northeast, approximately as far as today's Rendsburg-Flensburg motorway. Dithmarschen remained ice-free. Since a glacier releases large amounts of meltwater, especially in summer, wide streams of meltwater formed that led away from the glacier into the glacial valley of the Elbe. At that time, the world sea level was around 100 meters lower than it is today. One of these meltwater streams ran in what is now the lower Eider Valley and created a steep edge through erosion on the Dithmarscher Altmoräne. Due to earth flow caused by frost changes However, in the final phase of the Ice Age this was flattened. The actual valley floor of the Ice Age meltwater valley is still around five meters below the current meadows cultivated from fens. Along the path, this striking slope is well preserved and is often interspersed with springs over impermeable clay layers, which are covered by a different type of vegetation such as Sour grasses or alders are marked. The clay mined here was used in the late 19th and early 19th centuries In the 20th century, yellow bricks were burned in up to three brickworks and shipped in large quantities across the Eider. (…from information board)

A 40 m high ridge stood in the way of the planned railway line, which could not be bypassed. So you had to dig the route through the geest. In retrospect, this led to some landslides and large snow drifts in winter, so that trains derailed again and again. Today the old railway line is a beautiful, natural ravine.

Landscape formed by meltwater during the Ice Age.