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Reineberg

Castles in North Rhine-WestphaliaLübbeckeMindenMinden-LübbeckeWiehen Hills
Falk Oberdorf Heidkopf und Reineberg
Falk Oberdorf Heidkopf und Reineberg

The Reineberg is a hill on the Wiehen ridge, south of the town of Lübbecke. With a height of 275.9 m above sea level it is, from a topographical point of view, not a particularly impressive eminence in this part of the Wiehen Hills, because, in the immediate vicinity are considerably higher summits, such as the 320 m high Heidbrink just under 1 km to the south. East of the Reinberg on the other side of a valley bottom rises the Heidkopf, west of the Meesenkopf, on the summit of which there was once a fortification. 230 metres southwest of the summit lies the Wittekind Spring, that had a certain importance for the garrison of the castle at the summit, but today is just a small pond by a rock outcrop at the edge of a track. The Reineberg, which is the local hill for the town of Lübbecke, owes its significance to the fact that, until 1723, the year of its demolition, Reineberg Castle (German: Burg Reineberg or Reineburg) stood here.

Excerpt from the Wikipedia article Reineberg (License: CC BY-SA 3.0, Authors, Images).

Reineberg
Wittekindsweg,

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Geographical coordinates (GPS)

Latitude Longitude
N 52.29431 ° E 8.62847 °
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Address

Landesburg Reineberg

Wittekindsweg
32312 , Lübbecke
North Rhine-Westphalia, Germany
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Falk Oberdorf Heidkopf und Reineberg
Falk Oberdorf Heidkopf und Reineberg
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Heidbrink
Heidbrink

The Heidbrink is a hill which lies south of Lübbecke in central Germany and, at 319.6 m above sea level (NN), is the highest peak in the Wiehen Hills. It is also the highest elevation in the district of Minden-Lübbecke in the German state of North Rhine-Westphalia. Its height is commonly given as 320 metres. About 200 yards east of the summit is a transmission tower for television and radio links and a wayside hut for walkers. The mast has a paved access road from the B 239. The summit of the Heidbrink itself is in a small open area and, until 2008, was marked by a boulder. Due to the surrounding high trees the view is blocked to the north; to the south can parts of the Ravensberg Basin be seen. The Ronceva rises on the western slope of the mountain. To the north are the peaks of the Reineberg, 276 m above sea level, and the Heidkopf, 273 m. The southern flank of the mountain drops steeply to the hamlet of Ahlsen-Reineberg in the municipality of Hüllhorst. The ridgeway (Kammweg) passes over the top of the mountain. It forms the boundary between the town of Lübbecke and the municipality of Hüllhorst. The ridgeway runs as a footpath (the Wittekindsweg) along the Wiehen ridge from Osnabrück to Porta Westfalica, and links the Heidbrink with the Straußberg (276 m) in the east, and the Horsthöhe (275 m) and Kniebrink (315 m) in the west. To mark the highest point on the Heidbrink a five-ton sandstone block with strong iron deposits, typical of the local Wiehen Hills, was set up on 24 May 2008. According to information boards by the TERRA.vita Nature Park, members of the Lübbecke marketing association (Stadtmarketingverein) and the municipal curator of Hüllhorst have marked the route to the "highest stone" with their own symbol. These are sometimes signposts, sometimes coloured markings, on wayside tree trunks. The symbol, the letter "H" on a hill symbol, is meant to be linked with the name and the appearance of the hill. At the new summit stone are two tablets; the upper one describes the Heidbrink as the highest hill in the Wiehen range; the lower panel lists the sponsors of this marketing campaign. The new summit stone is not in the same place as the old and rather less imposing summit stone, but about 20 metres east. The original stone was removed during the work to set up the new one. But it appears that the original spot had marked the exact peak, but was not so obviously recognisable from the main footpath.

Mensinger Ravine

The Mensinger Ravine (German: Mensinger Schlucht) is a steep-sided valley in the Wiehen Hills in Central Germany that is situated on the territory of the town of Lübbecke in the district of Minden-Lübbecke. The ravine begins on the eastern slopes of the Wurzelbrink hill and runs northwards from there in a curve as far as the B 239 federal road. The ravine is around 800 metres long. The valley floor in its upper section lies at a height of around 210 m above NN and drops to 150 m above NN at the end of the valley, where the source of the Ronceva stream is found. In the ravine itself, although it was formed by erosive influences, there is no permanent stream - only during heavy rainfall at the "upper reaches of the Ronceva", so to speak, does any water flow. The valley floor itself is impassable on foot in places. However, immediately to the east is a forest track, that enables the valley to be walked from end to end in 15 minutes. The ravine is forested throughout. The Mensinger Ravine is a typical example of a Siepe, a narrow, wet, ravine-like, V-shaped valley in higher hills or low mountains with a source stream. (in the East Westphalian region of Ravensberg Land and in the Lipperland such a terrain feature is known as a Siek). The source streams in such a valley do not necessarily carry water all-year round, as in the case of that in the Mensiger Ravine, however, the stream is the reason the V-shaped valley was formed. It must however be taken into account for terrain shaping, that in the post ice age the water levels flowing out of the mountain ranges, including the Wiehen, were greater, so that streams were able to cut into the terrain much more than they do today. This is the reason the ravine is so deep despite the rather low levels of water flow on the ravine floor today.