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Rasta Dome

Basketball venues in GermanyGerman sports venue stubsIndoor arenas in GermanyLower Saxony building and structure stubsSports venues in Lower Saxony
Vechta (district)
RASTA Homep
RASTA Homep

Rasta Dome, stylized as RASTA Dome, is a sports arena in Vechta, Germany. The arena serves as the home venue of SC Rasta Vechta of the Basketball Bundesliga. The arena opened on 12 October 2012 and hosted its first event on 13 October 2012. In 2013, the arena, which had an original capacity of 2,000 spectators, was expanded to accommodate 3,140 fans in order to meet minimum size requirements for the Basketball Bundesliga.

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

Geographical coordinates (GPS)

Latitude Longitude
N 52.7332 ° E 8.2594 °
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Address

RASTA Dome

Pariser Straße 8
49377 , Stukenborg
Lower Saxony, Germany
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linkOpenStreetMap (195814685)

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Nearby Places

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).