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https://de.wikipedia.org/wiki/Kreisbahn_Norderdithmarschen

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

a typical field stone church, as there are some in this area. It dates from the 12th century. It has a very beautiful church interior. Lots of wood, quite colorful. I liked that very much. More at Wikipedia: https://de.wikipedia.org/wiki/St.-Marien-Magdalenen-Kirche_(Erfde)

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.

St. Marien-Magdalenen Church in Erfde The church in Erfde is located in the southwest of the church district. It is one of the three churches of the ev. luth. The parish of Stapelholm-Stapel. The natural boundaries of this parish are the rivers Eider, Treene and Sorge. They flow around the landscape like blue ribbons, villages, meadows and pastures. The Marien-Magdalenen church shows a simple Romanesque style, the walls mostly consist of partly very large boulders and are up to one meter thick. It was probably built in the 13th century. https://www.kirchenkreis-schleswig-flensburg.de/gemeinden/kreisgebiet-schleswig-flensburg/stapelholm/unsere-kirchen/st-marien-magdalenen-kirche-in-erfde.html

Best homemade cakes🍰, beautiful garden🌳🌻 with pond and decoration - SECRET TIP👍

Interesting historic church in Erfde.

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)