ヴェエーデの天然記念物・トップ20

The Herrenteich Pond is located in the heart of the carp town of Reinfeld. It was artificially created in the 12th century by Cistercian monks as a reservoir for the Heilsau River for fish farming. Carp are still bred here today. A four-kilometer circular trail around the Lower Herrenteich invites you to discover this special ecosystem. 16 stations along the adventure trail offer fun and a nature experience in one, sharpening your awareness of the special features of this natural area. In summer, you can enjoy the cool water at the lido. See: https://tourismus-stormarn.de/de/naturerlebnis/herrenteich-reinfeld-5

The Herrenteich in Reinfeld is a popular tourist destination. The approximately 55-hectare body of water is divided into the upper and lower Herrenteich. The upper Herrenteich remains a recognized nature reserve. The lower Herrenteich is home to, among other things, a hiking trail and an outdoor pool in the summer. Due to melting snow, the Herrenteich flooded in early March 2010. A temporary dam erected at the time due to construction work threatened to no longer hold the water masses. A breach of the dam would have flooded the entire hinterland. The Hamburg/Lübeck railway embankment would also have been affected. See: https://www.thw-badoldesloe.de/aktuelles/aktuelle-meldungen/artikel/vor-10-jahren-hochwassereinsatz-am-herrenteich-fachgruppen-wasserschadenpumpen-verhindern-stauwe

The 3.7 km long trail leads along the partially wooded shore of the Herrenteich lake. The east and west banks are connected by a bridge at the "Fischhuser Damm"—north of this bridge begins the "Oberer Herrenteich" nature reserve. See: https://reinfeld-aktiv.de/tag/reinfeld/page/6/

The Ihlsee is located in the northwestern part of the district town of Bad Segeberg on the northern edge of the Kleinniendorf district and is part of the designated Ihlsee and Ihlwald nature reserve. The origin of the lake has not been fully investigated. Either the depression was formed after the Ice Age due to dead ice or it was created as a sinkhole by the collapse of a cave in the Segeberg salt dome. Today the lake has an area of around 29 hectares and stretches 450 m from north to south and around 850 m from west to east; the shore is 2.25 km long. Along with the Bültsee and the Garrensee, the lake is one of the few nutrient-poor lakes in Schleswig-Holstein. The lake is located in a depression and has no inflow. It is fed only by groundwater and inflowing surface water (precipitation). To the north of the bathing area is the outflow that connects the lake to the Great Segeberg Lake. The lake can be walked around, but there is no path along the lake. There is a bathing area on the eastern shore that has existed for decades. The bathing water quality is regularly monitored and in recent years has been rated as very good to good. There is a residential area on the northern shore. On the western and southern sides, the Ihlwald, a swamp forest, dominates the shoreline. From 1911 to 1961, there was a Kiel-Segeberg narrow-gauge railway station at Ihlsee, the tracks of which were removed in 1962. The Ihlsee was declared a nature reserve in 1950 because of its special features. The lake is a particularly nutrient-poor body of water, which gives rise to rare flora. Today, the lake is part of the Ihlsee and Ihlwald nature reserve and has been part of the Natura 2000 protected area network since 2006. https://de.wikipedia.org/wiki/Ihlsee

Nice walk around the pond! With lots of cozy spots.

This is the bridge at Fischhuser Damm. The name suggests that a dam must once have connected the banks of the Herrenteich pond here. In 1960, pioneers from the Eutin riot police erected the first wooden bridge, which was recently replaced by a new steel structure. The "Oberer Herrenteich" nature reserve lies to the north of the bridge.

The Brenner Moor is the largest inland salt marsh in Schleswig-Holstein. It is located in the district of Stormarn in the town of Bad Oldesloe in the Trave lowlands and has been declared a nature reserve. What is special about the Brenner Moor are the brine springs that rise from a depth of approx. 500 meters and have their origin in a salt band that presumably stretches from Segeberg via Tralau and Bad Oldesloe to Lübeck. The plant communities and the animal world of the Brenner Moor are shaped in a special way by the unique occurrence of salt springs inland. The salty environment attracts plants that are otherwise only found near the coast, e.g. B. rush (Juncus gerardii) and beach trident (Triglochin maritima). In some places the water has a salinity that corresponds to that of the North Sea. In less saline parts of the nature reserve, reed beds, among other things, grow. https://metropolregion.hamburg.de/kulturlandschaften/4471072/brenner-moor/

It should read: Reinfeld - Herrenteich. Reinbeck is wrong, Reinbek is in the south of Stormarn, near Hamburg