グロース・ヴィッテンゼーの天然記念物・トップ20

After the burial forest, the path leads directly along the cliff edge, offering magnificent views across Eckernförde Bay... After storms, it can happen that sections of the coast are washed away and the path is temporarily no longer there.

Beautiful hike in August when the heather is in bloom.

Beautiful in August!

It is always worth hiking in the area of the Schlei, like here at the narrowest point of the Schlei, and enjoying the peace and quiet while hiking and listening to the birds.

The deepest point of the Windebyer Noor[2], at 13.6 metres, is in the north of the lake near the Eckernförde district of Carlshöhe; in the middle, the lake is eleven metres deep. The water of the Windebyer Noor is slightly saline (in different places between over one and a good two PSU[3]). Bulges of the Windebyer Noor are called Schnaaper Bucht (Snap Bugt), Norderhake (Nørrehage), Süderhake (Sønderhage), Südbucht (Sydbugt)[4] and Kochendorfer Bucht.[5] The Norderhake was the connecting arm of the Windebyer Noor to the Eckernförde city harbour.

The Windebyer Noor (obsolete: Eckernförder Noor, Schna(a)per Noor and Goos-Noor; Danish: Vindeby Nor, Low German: Winnebyer Noor, Winneby-Noor) is a 389 hectare inland lake in Schleswig-Holstein. It is located on the western edge of the town of Eckernförde, to whose municipal area it belongs. To the south and west, the eponymous municipality of Windeby borders the shore of the lake. Former residents of the lake were the municipality of Borby until its incorporation in 1934 (Borby exclave Schnaap) and the municipality of Gammelby until 1973 (Grasholz).

It has now happened: large sections of the path, which ran directly along the edge, have collapsed, taking numerous trees with them. Part of it has been cordoned off with barrier tape – which is now quite damaged. A narrow alternative path runs alongside the original one. It is very sad and frightening, but walkable – however, definitely not recommended for strollers or people with mobility impairments!

The Sorgwohlder inland dunes near Owschlag have been a nature reserve along the Sorge lowlands since 1936. It extends from Sorgwohld in a northeasterly direction. The dunes were formed in the late and post-glacial periods around 12,000 years ago. A constant ice wind blew the sand from the erosion edges, created by meltwater that had severely eroded the Owschlager Sander in Sorgetal, into mighty dunes. Today it can be assumed that parts of the Sorgwohlde inland dunes have been almost devoid of vegetation since the Ice Age. Humans have cultivated this landscape through grazing and farming since around 1000 AD. fundamentally shaped. The farmers in the sandy areas used the soil removed by pests to litter the stables and then fertilize their one-sidedly cultivated fields. Plowing and removing heather and other ground litter removed nutrients from the soil. This meant that the heather was always able to sprout new crops and germinate its sun-loving seeds better. The Ochsenweg also had an influence on the area. At Sorgwohld he crossed the worry. Large storage areas had to be available at such water points. The cattle kept churning up the ground. The Sorgwohlder inland dunes with their heaths and silver grass and lichen meadows, which are unique to Schleswig-Holstein and are home to a number of insects and spider species that are threatened with extinction. You can find further detailed information about the Sorgwohlder inland dunes here: http://www.owschlag.info/BUND/binnenduenen.htm