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Home > Art, Film & Photography > Pyrenaen: Marienerscheinungen Und Wallfahrt in Lourdes, Val D'Aran, Geologie Der Pyrenaen, Andorra
Pyrenaen: Marienerscheinungen Und Wallfahrt in Lourdes, Val D'Aran, Geologie Der Pyrenaen, Andorra

Pyrenaen: Marienerscheinungen Und Wallfahrt in Lourdes, Val D'Aran, Geologie Der Pyrenaen, Andorra


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About the Book

Dieser Inhalt ist eine Zusammensetzung von Artikeln aus der frei verfugbaren Wikipedia-Enzyklopadie. Seiten: 30. Nicht dargestellt. Kapitel: Marienerscheinungen und Wallfahrt in Lourdes, Val d'Aran, Geologie der Pyrenaen, Andorra, Nationalpark Aiguestortes i Estany de Sant Maurici, Canaveilles-Gruppe, Saint-Jean-Pied-de-Port, Pays d'Aillou, Burg Montsegur, Hohle von Niaux, Gallego, Vall de Nuria, Nationalpark Ordesa y Monte Perdido, Ossau-Iraty Brebis-Pyrenees, Bearn, Nationalpark Pyrenaen, Yesa-Talsperre, Baztan, Bagneres-de-Luchon, Grotte des Canalettes, El Turbon, Astun, Cirque de Gavarnie, Laboratorio subterraneo de Canfranc, Plateau de Beille, Gavarnie-Falle, Sierra de Guara, La Mongie, Sierra de Gratal. Auszug: Die Geologie der Pyrenaen wird bestimmt durch die Zugehorigkeit des rund 430 Kilometer langen, Frankreich und Spanien trennenden, polyzyklischen Gebirgszuges zum riesigen alpidischen Gebirgssystem. Die Ost-West-verlaufende Pyrenaen-Kette (Streichen 110 ) entstand aufgrund der Kontinentalkollision zwischen dem Mikrokontinent Iberia und dem sudwestlichen Auslaufer der Eurasischen Platte (Sudfrankreich). Die Annaherung der beiden Kontinente erfolgte ab dem Beginn der Oberkreide (Albium/Cenomanium) vor rund 100 Millionen Jahren und fuhrte im Verlauf des Palaogens (Eozan/Oligozan) zwischen 55 und 25 Millionen Jahren zur Heraushebung des Orogens. Seit diesem Zeitpunkt unterliegt das Gebirge neben isostatischen Ausgleichsbewegungen hauptsachlich starker Abtragung. Die Pyrenaen besitzen im Profil eine asymmetrische Facherstruktur mit steileren Einfallswinkeln auf der franzosischen Nordseite. Die Gebirgskette ist nicht allein kompressiven Ursprungs, sondern besitzt auch eine bedeutende sinistrale Scherkomponente. Die intrakontinentale Gebirgskette der Pyrenaen ist der nordwestlichste Zweig des rund 12 000 Kilometer langen alpidischen Gebirgssystems. Im engeren Sinne erstrecken sich die Pyrenaen uber 430 Kilometer in Westnordwest-Ostsudost-Richtung (N 110) vo...


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Product Details
  • ISBN-13: 9781159278670
  • Publisher: Books LLC, Wiki Series
  • Publisher Imprint: Books LLC, Wiki Series
  • Height: 246 mm
  • No of Pages: 32
  • Spine Width: 2 mm
  • Weight: 77 gr
  • ISBN-10: 1159278679
  • Publisher Date: 28 Aug 2011
  • Binding: Paperback
  • Language: German
  • Returnable: N
  • Sub Title: Marienerscheinungen Und Wallfahrt in Lourdes, Val D'Aran, Geologie Der Pyrenaen, Andorra
  • Width: 189 mm


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