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Babilonie

Hill forts in GermanyIron AgeLa Tène cultureLübbeckeMinden-Lübbecke
Wiehen Hills
Obermehnen
Obermehnen

The Babilonie is a hillfort of the La Tène culture at a height of 255.6 metres above sea level on the northern edge of a rounded hill in the Wiehen Hills above the Lübbecke village of Obermehnen in the district of Minden-Lübbecke in the German state of North Rhine-Westphalia. The name is derived from the Germanic baben in the lon i.e. "up in the woods". The wedge-shaped, double-rampart system, which descends from south to north with the slope, was investigated archaeologically in the first half of the last century, especially by Friedrich Langewiesche, who assessed it as a refuge castle. Ceramic and even metalwork finds indicate that it belongs to the La Tène culture in the pre-Roman Iron Age, e vorrömische Eisenzeit, therefore probably part of an extensive trading network. The fortification has an area of over 12 hectares. The first mapping of this hilltop, which was exceptionally well-suited to the establishment of a large hillfort with its spring high up the hills, was carried out after 1880.Ceramic finds from the Saxon-Frankish period have also been discovered. According to Paul Höfer there is a legend that refers to Wittekind.

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

Babilonie
Babilonieweg,

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Geographical coordinates (GPS)

Latitude Longitude
N 52.27667 ° E 8.57667 °
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Address

Babilonieweg
32312 , Obermehnen
North Rhine-Westphalia, Germany
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Obermehnen
Obermehnen
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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.