Cologne Bay
Cologne Bay | |||
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Systematics according to | Handbook of the natural spatial structure of Germany | ||
Greater region 1st order | North German Lowlands | ||
Greater region 2nd order | Central North German Lowland | ||
Main unit group | 55 → Lower Rhine Bay |
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Natural space |
551 → Cologne Bay |
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Geographical location | |||
Coordinates | 50 ° 56 '17 " N , 6 ° 57' 25" E | ||
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state | North Rhine-Westphalia | ||
Country | Germany |
As Cologne Bay (rarely Cologne-Bonn Bay ) which is low terraces - level of the Rhine , made up, of Bonn in the southeast northwestward over Cologne until immediately before Dusseldorf and Neuss draws.
It is located in the southwest of North Rhine-Westphalia and forms the central part of the Lower Rhine Bay , which sinks into the Rhenish Slate Mountains from the northwest . To the east and west of the Cologne Bay, the adjoining partial landscapes of the Lower Rhine Bay rise in terraces towards the Southern Mountains (in the east) and the Eifel (in the west).
Occasionally the term Cologne Bay is used synonymously with the entire Lower Rhine Bay or the agglomeration of the city of Cologne.
geography
Location and limits
The Cologne Bay is framed by the wider landscapes of the Lower Rhine Bay. The border is particularly clear on the west side with the bounding landscape of the Ville and its eastern slope, the promontory . On the east side, the area of the surrounding heather terraces does not rise so clearly, but the change to the heather is particularly noticeable. To the northwest, the entire bay opens up along the Rhine and merges into the Lower Rhine Lowland , to which the Münsterland chalk basin of the Westphalian Bight sinks from the east . Further to the northwest, the Rhine and Maas valleys gradually merge.
Natural structure
In terms of nature , the Cologne Bay represents a main unit (three-digit) and is divided into sub-units (decimal places ) as follows:
- 55 (to 55 Lower Rhine Bay )
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551 Cologne Bay in the narrower sense ( Cologne-Bonn-Rhine plain and central terrace slabs on the left bank of the Rhine )
- 551.0 Siegburg Bay
- 551.00 Menden-Hangelarer Terraces
- 551.01 Sieg-Agger lowland
- Michaelsberg ( singularity )
- Wolsberge (singularity)
- 551.1 Lower terrace level on the right bank of the Rhine ( Lower terrace on the right bank of the Rhine )
- 551.10 Mülheimer Rheinebene ( Mülheimer-Porzer low terrace )
- 551.11 Benrath Rhine plain
- 551.12
- 551.0 Siegburg Bay
- 551.2 Rheinaue
- 551.20 Cologne-Bonn Rhine plain
- 551.21 Dormagener Rheinaue
- 551.3 Lower terrace level on the left bank of the Rhine ( Lower terrace on the left bank of the Rhine )
- 551.30 Southern Cologne Rhine Plain ( Cologne-Bonn Lower Terrace )
- 551.31 Northern Cologne Rhine Plain
- 551.32 Mühlen- and Knechtstedener Busch
- 551.4 Middle terrace slabs on the left bank of the Rhine ( Loosen terrace plates on the left bank of the Rhine )
- 551.40 Brühler loess plate
- 551.41 Brauweiler Loess Plate
- 551.42 Rommerskirchen loess plate
- 551.43 Allrath-Neukirchen clay plate
- 551.5 Godesberg Rhine valley funnel
- Castle hill of Godesburg (singularity)
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551 Cologne Bay in the narrower sense ( Cologne-Bonn-Rhine plain and central terrace slabs on the left bank of the Rhine )
Culture
Due to the function of the Rhine as a mode of transport since ancient times, the bay is heavily populated and shaped by people. In recent times this traffic situation has also been used by industry, particularly in the peripheral areas of the agglomerations .
climate
As the southernmost foothills of the Lower Rhine lowlands, the Cologne Bay, protected by the surrounding mountains, is one of the warmest regions in Germany with average annual temperatures between 10 and 11 ° C.
The maritime climate is influenced by the Gulf Stream across the Atlantic and the proximity to the North Sea. Mild winters and moderate summers correspond to this situation.
In turn, the bay location can lead to inversion weather situations in which there is hardly any air exchange and pollutant concentrations in the air rise.
Geological history of development
About 30 million years ago parts of the Rhenish Slate Mountains sank, and a lowland area formed, which the Rhine alternately accumulated or carried away with gravel. The imprint of the immediate Cologne Bay, the lower terrace, took place in the geologically most recent era. Often, former rivers can still be seen on it, for example the Worringer Bruch . The arable land is characterized by the alternation of gravelly areas with more fertile stretches of alluvial clay.
See also
Web links
Individual evidence
- ^ Emil Meynen , Josef Schmithüsen : Handbook of the natural spatial structure of Germany . Federal Institute for Regional Studies, Remagen / Bad Godesberg 1953–1962 (9 deliveries in 8 books, updated map 1: 1,000,000 with main units 1960).
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↑ Various authors: Geographische Landesaufnahme: The natural spatial units in single sheets 1: 200,000 . Federal Institute for Regional Studies, Bad Godesberg 1952–1994. → Online maps
- Sheet 108/109: Düsseldorf / Erkelenz (Karlheinz Paffen, Adolf Schüttler, Heinrich Müller-Miny 1963; 55 pages)
- Sheet 122/123 *: Cologne / Aachen (Ewald Glässer 1978; 52 pages)
- ↑ a b Institute for Regional Studies (ed.); Heinrich Müller-Miny (arrangement): Geographical and regional explanations for the topographical map 1: 50000 . 1. Delivery, self-published by the Federal Institute for Regional Studies and Spatial Research, Bad Godesberg 1963, p. 33.
- ↑ a b c d e Designation according to the Cologne journal
- ↑ Adolf Schüttler, one of the three authors of Blatt Düsseldorf-Erkelenz , counts the Hildener Sandniederterrasse as part of the main unit 550 (or 550.1) because of its transfer.
- ^ Heinrich Müller-Miny: considerations on the natural spatial structure . In: Institute for Regional Studies (Ed.): Reports on German Regional Studies . Volume 28, Issue 2 (March 1962), self-published by the Federal Institute for Regional Studies and Spatial Research, Bad Godesberg 1962, pp. 258–279 (here: 276).
- ↑ Which climate characterizes the Cologne Bay? (City of Cologne, accessed March 7, 2015)