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The ''' |
The '''Viennese Basin''' (German: ''Wiener Becken'', Czech: ''Vídeňská pánev'', Slovak: ''Viedenská kotlina'') is a [[sedimentary basin]] between the [[Alps]] and the [[Carpathian Mountains]]. More than 50% of the Viennese basin is located in [[Lower Austria]], the rest is in the [[Czech Republic]] and [[Slovakia]]. |
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[[Image:Chvojnica hills near Unin.jpg|thumb|right|Chvojnice Hills in Slovakia]] |
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The fairly level area has the shape of a [[ |
The fairly level area has the shape of a [[spindle]], over an area of 50 kilometres by 200 kilometres. |
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It forms a defensible valley from attacks from downstream on the [[Danube]], ([[Hungary]]). |
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The [[Battle of Vienna]], 1529, had Ottoman Turks against the walls of the city. |
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Parts: |
Parts: |
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*The |
*The Viennese Basin proper. The part within the Czech Republic is called Dolnomoravský úval (the [[Lower Moravian Vale]]), whilst that within Slovakia is called Borská nížina (the [[Bor Lowland]]) |
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*[[Marchfeld]] in Austria |
*[[Marchfeld]] in Austria |
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*[[Leitha Mountains]] (Leitha-Gebirge) in Austria |
*[[Leitha Mountains]] (Leitha-Gebirge) in Austria |
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==Geology== |
==Geology== |
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The Vienna Basin formations are a series of [[Sedimentary rock|sedimentary layers]] that were deposited in the [[Neogene]]. |
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The Vienna Basin formations are a series of [[Sedimentary rock|sedimentary layers]] that were deposited in the [[Neogene]]. It was formed by [[Pull Apart Basin|pull apart]] mechanism<ref>Plašienka, D., Grecula, P., Putiš, M., Kováč, M. a Hovorka, D., 1997: ''Evolution and structure of the Western Carpathians: an overview.'' Mineralia Slovaca - Monograph, Košice, s. 1 – 24</ref> and the Vienna Transform fault on which the Vienna Basin lies remains seismically active. Significant earthquakes that propagated across the Vienna Basin include the [[1590 Neulengbach earthquake|Neulengbach earthquake]] of 1590, and the strong temblor that hit [[Carnuntum]] in the mid-4th century. |
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== References == |
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{{Reflist}} |
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==External links== |
==External links== |
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* [http://www.weinvierteldac.at/rte/upload/geologie/geol.karte_geol._map_weinviertel_2006_150dpi.gif "Simplified Geological Map of the Weinviertel region"] |
* [http://www.weinvierteldac.at/rte/upload/geologie/geol.karte_geol._map_weinviertel_2006_150dpi.gif "Simplified Geological Map of the Weinviertel region"] |
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{{ |
{{Austria-geo-stub}} |
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[[Category: |
[[Category:Geography of Austria]] |
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[[Category: |
[[Category:Geography of Slovakia]] |
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[[Category: |
[[Category:Geography of the Czech Republic]] |
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[[Category:Sedimentary basins of Europe]] |
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[[cs:Vídeňská pánev]] |
[[cs:Vídeňská pánev]] |
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[[da:Wienerbækkenet]] |
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[[de:Wiener Becken]] |
[[de:Wiener Becken]] |
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[[fr:Bassin de Vienne]] |
[[fr:Bassin de Vienne]] |
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[[la:Sinus Vindobonensis]] |
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[[lt:Vienos baseinas]] |
[[lt:Vienos baseinas]] |
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[[ |
[[nn:Wien-bekkenet]] |
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[[no:Wienbekkenet]] |
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[[nn:Wienerbekkenet]] |
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[[pl:Kotlina Wiedeńska]] |
[[pl:Kotlina Wiedeńska]] |
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[[ru:Венский бассейн]] |
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[[sk:Viedenská kotlina]] |
[[sk:Viedenská kotlina]] |
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[[sv:Wienerbäckenet]] |
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[[uk:Віденський басейн]] |
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[[zh:維也納盆地]] |
[[zh:維也納盆地]] |
Revision as of 06:34, 14 February 2011
The Viennese Basin (German: Wiener Becken, Czech: Vídeňská pánev, Slovak: Viedenská kotlina) is a sedimentary basin between the Alps and the Carpathian Mountains. More than 50% of the Viennese basin is located in Lower Austria, the rest is in the Czech Republic and Slovakia.
The fairly level area has the shape of a spindle, over an area of 50 kilometres by 200 kilometres.
Parts:
- The Viennese Basin proper. The part within the Czech Republic is called Dolnomoravský úval (the Lower Moravian Vale), whilst that within Slovakia is called Borská nížina (the Bor Lowland)
- Marchfeld in Austria
- Leitha Mountains (Leitha-Gebirge) in Austria
- Chvojnice Hills (Chvojnická pahorkatina) in Slovakia
The Bor Lowland and Chvojnice Hills are known collectively as Záhorská nížina (the Záhorie Lowland).
Geology
The Vienna Basin formations are a series of sedimentary layers that were deposited in the Neogene.