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教会は1871年から1872年にかけて赤レンガで建設され、1873年に奉献されました。破壊されなかった古い墓所の石壁は、現在の教会の東壁の基礎壁となっています。東壁は、その奥にある祭壇室へと、コーラスアーチを通して開かれています。 地図 » 地図上で

.-Luth. Schlamersdorf教会 Schlamersdorf教会は、ベルリン、シュラマースドルフの村々と約1700人の教会員を持つシードルフの荘園区を包含しています。

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.