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이 교회는 1871년부터 1872년까지 붉은 벽돌로 지어졌으며 1873년에 축성되었습니다. 파괴되지 않은 오래된 무덤의 동쪽 벽은 현재 교회의 동쪽 벽의 기초입니다. 동쪽 벽은 합창석 아치를 통해 그 뒤에 있는 제단 공간으로 열립니다. 지도 » 지도에서

.-Luth. Schlamersdorf 교회 Schlamersdorf 교회는 베를린, Schlamersdorf 마을과 약 1700명의 교구민을 가진 Seedorf 영지구를 포함합니다.

I passed through there two years ago on my "Timmd-Uetersen-a02" tour. The tour is part of the return trip from the cycling trip to Plön, which several people took with me.

The path directly along the Perdoel estate to the bridge over the Alte Schwentine is private and closed. The lord of the manor does not like hikers using this path.

Lake Schmalensee is located west of the town of Schmalensee and borders the Holstein Switzerland Nature Park. It covers approximately 90 hectares and is up to 7.5 meters deep. It is part of the Bornhöved Lake Chain, which consists of six lakes and is also part of the Wankendorf Lake District. Lake Bornhöved is located south of Lake Schmalensee, and in the immediate vicinity; the two are connected by a 100-meter-long branch canal. There is a swimming area on the southeastern shore of the lake.

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.