バルクテハイデの天然記念物・トップ20

Rodenbeker Quellentag - Gasthaus Quellhof, great place to stop for refreshments with beer garden

The Rodenbek is a river that flows into the Alster in the Rodenbeker Quellental nature reserve. The idyllic Rodenbeker pond along its course is managed by the Rahlstedt sports fishing association from 1934 e.V. and is the habitat of numerous fish species, such as carp, eel and perch. kulturlotse.de/ort/rodenbeker-teich-3806401676914271620

Cheerful birdsong accompanies you through the beautiful deciduous forest. The frogs are croaking in the pond.

The Brenner Moor is the largest salt marsh in inland Schleswig-Holstein. The salinity of the salt springs partially reaches that of the North Sea. A jewel of nature but very busy on weekends. Still a real highlight. The crossing is only possible thanks to the laid planks. However, cycling is prohibited

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/

The Rodenbeker Quellental nature reserve is an 84-hectare glacial meltwater river system in northeast Hamburg. It lies in the former edge area of the Vistula glaciation. Locally there are elevations in the form of ground moraines. The site elevation is between 15 and 20 meters above mean sea level. The site was granted protected status on January 25, 1977, originally measuring 47 hectares. On July 26, 2011, the Hamburg Senate announced an expansion by 37 hectares to 84 hectares. In the Quellental there are extensive deposits from an ice reservoir, which are now cut through by various smaller basins, small rivers. These are the Rodenbek, the Bredenbek, the Lottbek, the Mühlenbek and other small streams. All flow in an east-west direction to the Alster, a northern tributary of the Elbe. The formation of the Rodenbeker Quellental began in the Weichselian Ice Age, when the Bredenbek Glacier slowly retreated and the meltwater at the base of the glacier found its way to the Alster. The current appearance of the spring valley is also due to spring erosion. (Source: Wikipedia)

Great moor and beautiful boardwalk! Tip: 🅿️ at the Kleingartenverein

The diverse landscape north-west of the town of Bad Oldesloe invites you to take a contemplative and, in view of the large number of natural history features, also eventful and informative tours. Several large-scale salt springs rising from great depths of salt domes have created very rare habitats for salt plants (halophytes) and a particularly adapted animal world here inland. The 24-hectare Brenner Moor nature reserve includes the largest inland salt pan in Schleswig-Holstein. The area is accessible by boardwalks. Ten experience stations provide in-depth information on the leaflets provided and encourage further research. The waterlogging of the Wolkenweher Niederung fulfills the goals of the European Water Framework Directive and also the requirements of the Habitats Directive. Source: environmental data.landsh.de