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Cloppenburg

CloppenburgCloppenburg (district)Pages including recorded pronunciationsPages with German IPAPages with Saterland Frisian IPA
Towns in Lower Saxony
Cloppenburg in CLP
Cloppenburg in CLP

Cloppenburg (German: [ˈklɔpm̩ˌbʊʁk] ; Low German: Cloppenborg; Saterland Frisian: Kloppenbuurich [ˈklɔpənˌbuːrɪx]) is a town in Lower Saxony, Germany, capital of Cloppenburg District and part of Oldenburg Münsterland. It lies 38 km south-south-west of Oldenburg in the Weser-Ems region between Bremen and the Dutch border. Cloppenburg is not far from the A1, the major motorway connecting the Ruhr area to Bremen and Hamburg. Another major road is the federal highway B213 being the shortest link from the Netherlands to the A1 and thus to Bremen and Hamburg. The town had strong cultural links with St Munchins Parish in Limerick, Ireland from the 1970s to the 1990s. During this period many groups of teens/young adults from both areas visited and were hosted by families from the other area.

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

Cloppenburg
Osterstraße,

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Geographical coordinates (GPS)

Latitude Longitude
N 52.85 ° E 8.05 °
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Address

Osterstraße 84
49661 , Hemmelsbühren
Lower Saxony, Germany
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Cloppenburg in CLP
Cloppenburg in CLP
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Cloppenburg Geest

The Cloppenburg Geest (German: Cloppenburger Geest) is a geest region near the town of Cloppenburg in North Germany and the centre of the Saalian glaciation Upper Pleistocene terrain of the Ems-Hunte Geest region. The meltwater sands (Schmelzwassersande) of the advancing ice sheet covered the old terrain with outwash sands (Vorschüttsande). Woldstedt (1955: 159) spoke about underlying sands that, in the "Cloppenburg-Bassum Geest", belonged to the Elster glaciation. A covering of boulder clay was deposited over the outwash sands during the Saale glaciation, or more precisely the Drenthe stage. A series of meltwater valleys characterises the surface of the Cloppenburg Geest, something that was vital to the emergence of the river network. "Numerous parallel, flat channels cross the terrain and so create a landscape of parallel ridges" writes Woldstedt (1955: 158). There are two opposing theories for the formation of the rivers. Hausfeld (1983; 1984) put their emergence down to large cracks in the Drenthe ice sheet, through which meltwaters flowed as the glacier thawed, cutting through the ground moraines and down into the outwash sands. Woldstedt (1956) spoke of channels (Rinnen) in another connexion. The advancing ice followed the depth contours, conserving and deepening them. When the ice sheet retreated, dead-ice (Toteis) remained deep in these channels; it was their thawing that then enabled the rivers to flow down their old valleys. During the marine regression of the Weichselian glaciation that ended about 12,000 years ago, in which the northwest German plain was not covered by ice, the rivers of the Cloppenburg Geest cut deeply into the valley sands. At that time the windborne and dune sands were formed especially as the area around the perimeter dried out. The climate of the post-glacial period was moister and warmer. The rise in sea level, the base level for river erosion, probably led to a rise in the water table in the geest depression (Roeschmann, 1971: 189). In the valleys vast fen peats formed, whilst on the valley edges and the larger basins raised bogs were formed (Hausfeld, 1983: 245).