Negernbötel: Moorland and Historic Traces

In Negernbötel, historic traces meet moorland and waterways. This gives you a range of themes to explore as you plan your trip: the development of the village, evidence of former fortifications, and the landscape around Kiebitzholmer Moor and the Faule Trave.

Historic Traces from the Neolithic to the Baroque Period

Negernbötel was first mentioned in a document on 10 October 1198. The name element Botele or Bötel probably derives from a Low German word for a dwelling or settlement. The long barrows south of the road between Negernbötel and Hamdorf contain megalithic tombs from the Neolithic period, dating to around 3500 BC.

Military structures also form part of the area’s history. Several earthworks and defensive structures are particularly visible east of the new community centre. Banks and ditches in the woods around Negernbötel are interpreted as military structures. East of the motorway, the historic defensive system comprises two lines of defence and redoubts. The redoubts measure 30 by 30 metres on the outside and 15 by 15 metres on the inside; they were designed to protect 20 to 30 soldiers.

Remains of Baroque-era military structures extend across an area of ten square kilometres north of Negernbötel and Hamdorf. The long barrows point to a distant prehistoric past, while the fortifications tell of later military use. Visitors interested in local history will therefore find several themes from different periods here, without them being conflated into a single complex.

Faule Trave: Source Area and Trails

At the crossing of the Faule Trave, an information board explains this small tributary of the Trave. A circular trail in Negernbötel includes the source area of the Faule Trave. There, relatively steep slopes surround the spring area, and the trail offers views across the wet lowland.

A 1.6-kilometre link for cyclists between Negernbötel and Hamdorf, running along the K 91 district road, was officially opened on 19 June 2026. Its route and length differ from those of the circular trail by the source area. If you are planning to use the cycle link on a future trip, check its infrastructure status again.

Moorland and Nature

Kiebitzholmer Moor is located in Negernbötel. The Kiebitzholmer Moor and Trentmoor SAC covers 535 hectares in Schleswig-Holstein. Its habitats include transition mires and quaking bogs, as well as degraded raised bogs that can still regenerate naturally. The area is therefore defined by both its different types of mire and the potential for natural regeneration.

Some peat cuttings in Kiebitzholmer Moor contain raised-bog vegetation, including sphagnum mosses, cottongrass and bog myrtle. The treeless lowlands provide breeding and feeding grounds for meadow birds, including meadow pipits, whinchats and skylarks. Cranes are occasionally seen, although sightings vary by season. The SAC is also designated for the great crested newt (Triturus cristatus).

The land has a history of use, too: in 1976, Galloways brought from Scotland were first used in Schleswig-Holstein as landscape managers at Kiebitzholmer Moor. Clearly visible steep edges remain along the valley. The watershed between the North Sea and the Baltic Sea also runs through the moorland. The Brandsau flows east towards the Baltic Sea, while the Rothenmühlenau drains into the North Sea via the Stör. This means that the water landscape described here has two distinct drainage directions.

Discover more destinations: Hasenmoor, Todesfelde, Blunk, Seedorf, Hagen, Fahrenkrug, Schmalensee, Kaltenkirchen

For the regional travel overview: Segeberg.