보사우 주변 최고의 교통량 없는 자전거 라이딩 코스

The path leads directly past the bathing area.

Today a hotel, formerly a huge farm complex.

Bad Segeberg can be seen in the distance.

A grassy path leads along the lake to the bathing area, and there is also a parking lot above the bathing area. The bathing area has a jetty and is marked as a non-swimmer and swimmer zone. Watch out for seaweed in the swimming area. There is a small sandy beach, a large lawn, and benches for relaxing, as well as restrooms and a changing room. The lake is 23 hectares in size and 2.2 meters deep and is a channel lake (formed by thawed meltwater during the last ice age).

Swimming area on the Großer Plöner See (Great Plön Lake) with a sandy beach, playground, and sunbathing lawn. The long, sandy beach is the ideal swimming spot for families. A sunbathing lawn, benches, a hammock, a slide, mini-golf, and a small playground invite you to linger. The water is gently sloping and marked with a non-swimmer's boundary. Shady spots and a jetty into the water are available, as are changing facilities and restrooms.

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.