ゼーゲベルクのおすすめツーリングルート

素晴らしい休憩場所

The path leads directly past the bathing area.

The church in Stellau is a simple fieldstone building dating from around 1230. Over the centuries, the building underwent several structural alterations; the chancel was demolished in 1634 and again in 1651. From the 17th to the 19th centuries, the building was reinforced with slanted buttresses at the corners. A wooden bell tower was erected in 1851. The church furnishings include a medieval crucifix and a figure of a bishop, a sandstone baptismal font donated by Heinrich Rantzau in 1593, and a wooden pulpit from 1560, which was repainted around 1640/50. The organ dates from 1844/45. Contact: https://www.kk-rm.de/der-kirchenkreis/einrichtungen/institution/institution/ev-luth-kirchengemeinde-stellau/

The Langenrade windmill (also known as the "Sventana" windmill) is an impressive historical monument in the municipality of Ascheberg, very close to Plön.

The only fully functional of the three windmills within the Holstein Switzerland Nature Park is located in Ascheberg-Langenrade. The windmill, named "Sventana," was built in 1860 in Kleinmühlen near Plön. It has stood in Ascheberg only since 1890, replacing a predecessor that burned down. In 1982, three couples with a passion for windmills decided to restore it to working order. After considerable financial investment and many hours of labor, the single-story smock mill has been operational and flying again since 1990. The restoration of the mill's sails was financially supported, among other things, by state funds for nature parks.

a very idyllic tour at 6 a.m.

Peat cutting, i.e., the above-ground extraction of peat, is no longer economically viable today. Peat as a fuel has largely been replaced by other high-energy fossil fuels. Many large-scale peatlands suitable for industrial extraction have now been drained. New peat cutting areas are only permitted under strict conditions. Raised bogs have an important regulatory effect on the water balance due to the large amounts of precipitation they can absorb. The preservation of the original habitats serves landscape conservation and species protection, as most species of peatland flora and fauna are considered threatened or critically endangered. Bogs grow extremely slowly; an intact peat body increases in thickness by only one millimeter per year. It therefore takes a thousand years for a one-meter-high layer of peat to form. Thus, bog areas recover very slowly during restoration attempts.

The reclamation of the Himmelmoor began around 1780. Its edges were divided into 1,000 to 5,000 square meter plots and transferred to farmers from neighboring villages for peat extraction. Industrial peat extraction began in the 1870s. Peat was now also extracted from the center of the moor using machines. Peat excavators extracted the black peat, compressed it, and divided it into sods. Turning the drying sods was increasingly done by machine, as was the collection of the dry peat. The low-energy fuel was packaged and loaded at the peat works.