퀴렌 주변 최고의 그래블 라이딩 코스

훌륭한 목가적인 길

Imposing entrance gate to the pretty monastery courtyard

People have found comfort and hope in this prayer room for over 50 years. You are warmly welcome to join us for worship or family gatherings. Hikers, cyclists, nature lovers, and athletes will also find a space open day and night.

A winding path through beautiful countryside. Unfortunately, they didn't skimp on the coarse gravel. Not recommended for tires with high rims.

As early as 1264-1289, Neuwühren appeared in the "Kiel City Register" under the name de Javorn, which derives from the Old Polabite (a Slavic root) word Javor for maple. Shortly thereafter, it was renamed Nî-Jaworn, indicating that, as was common at the time, a German "new" village was founded alongside the Wendish one for the purpose of colonization. By 1460, the village was already called Nyenwörden—it was now only a short distance to Neuwühren. Like most of the surrounding villages, Neuwühren belonged to the Preetz Monastery. After the construction of the church there, Neuwühren became part of the Elmschenhagen parish. In 1931, the village was incorporated into the newly founded municipality of Pohnsdorf.

The lake was first mentioned in a document in 1075 in a description of the Limes Saxoniae by Adam of Bremen. The village was first mentioned in 1347, when the knight Nikolaus Splyth pledged his estate, including the village of Stocksee, to Reinfeld Monastery. From 1640 to 1649, Stocksee was owned by the noble Brockdorff family. In 1649, Duke Joachim Ernst (Schleswig-Holstein-Sonderburg-Plön), the first Duke of the Duchy of Schleswig-Holstein-Sonderburg-Plön, acquired Stocksee.[6]

On October 1, 1937, the municipality of Stocksee was merged with the neighboring village of Damsdorf under the name Stocksee. In 1948, the municipal council decided to separate the municipalities again, and this decision was implemented on March 31, 1951.[8][9] In the 1980s, divers found a roughly 700-year-old dugout canoe in the lake, indicating a longer settlement history in the village.

Today's lake fills a deeply incised glacial tongue basin from the Weichselian glaciation. This basin was formed by the advance of various glaciers, which carved out large basins in the soft soil and deposited the material laterally. This formation resulted in the lake's shores being relatively steep, and the reed beds along the shores are relatively narrow. The lake contains three islands (Großrethberg, Kleine Insel, and Lange Insel) and a peninsula, which, like the shoreline, are predominantly covered in alder swamp forests. In higher elevations, these wetland forests transition into extensively managed beech forests.