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The '''Vienna Basin'''<ref>Rees, Henry (1974). ''Italy, Switzerland and Austria. A Geographical Study.'' Harrap, London, ISBN 0-245-51993-9.</ref> (German: ''Wiener Becken'', Czech: ''Vídeňská pánev'', Slovak: ''Viedenská kotlina'', Slovenian: ''Dunajska kotlina'') is a [[sedimentary basin]] between the [[Alps]] and the [[Carpathian Mountains]]. More than 50% of the Vienna Basin is located in [[Lower Austria]], the rest is in [[Vienna]], the [[Czech Republic]] and [[Slovakia]].
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]].
[[Image:Chvojnica hills near Unin.jpg|thumb|right|Chvojnice Hills in Slovakia]]


The fairly level area has the shape of a [[spindle (textiles)|spindle]], over an area of 50 kilometres by 200 kilometres.
The fairly level area has the shape of a [[spindle]], over an area of 50 kilometres by 200 kilometres.

It forms a defensible valley from attacks from downstream on the [[Danube]], ([[Hungary]]).

The [[Battle of Vienna]], 1529, had Ottoman Turks against the walls of the city.


Parts:
Parts:
*The Vienna 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]])
*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
*[[Marchfeld]] in Austria
*[[Leitha Mountains]] (Leitha-Gebirge) in Austria
*[[Leitha Mountains]] (Leitha-Gebirge) in Austria
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==Geology==
==Geology==
The Vienna Basin formations are a series of [[Sedimentary rock|sedimentary layers]] that were deposited in the [[Neogene]].
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.

== References ==
{{Reflist}}


==External links==
==External links==
* [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"]


{{coord missing|Austria}}
{{Austria-geo-stub}}


[[Category:Landforms of Austria]]
[[Category:Geography of Austria]]
[[Category:Landforms of Slovakia]]
[[Category:Geography of Slovakia]]
[[Category:Landforms of the Czech Republic]]
[[Category:Geography of the Czech Republic]]
[[Category:Sedimentary basins of Europe]]


[[cs:Vídeňská pánev]]
[[cs:Vídeňská pánev]]
[[da:Wienerbækkenet]]
[[de:Wiener Becken]]
[[de:Wiener Becken]]
[[fr:Bassin de Vienne]]
[[fr:Bassin de Vienne]]
[[la:Sinus Vindobonensis]]
[[lt:Vienos baseinas]]
[[lt:Vienos baseinas]]
[[nl:Weense bekken]]
[[nn:Wien-bekkenet]]
[[no:Wienbekkenet]]
[[nn:Wienerbekkenet]]
[[pl:Kotlina Wiedeńska]]
[[pl:Kotlina Wiedeńska]]
[[ru:Венский бассейн]]
[[sk:Viedenská kotlina]]
[[sk:Viedenská kotlina]]
[[sv:Wienerbäckenet]]
[[uk:Віденський басейн]]
[[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 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.