Wednesday, July 8, 2009

Côte Sauvage. Wild Coast of Quiberon Peninsula.

The Quiberon Peninsula was originally an island and has been joined to the mainland by the accumulation of sand washed up by the sea. Its wild scenery - particularly impressive along the Côte Sauvage on the western side - attracts many visitors. The cliffs are made up of two-mica granites. Geologists have newly interpreted the Quiberon area in the Variscan belt of South Brittany (France) as a crustal shear zone and have postulatred Carboniferous extension tectonics as evidenced by normal faults, high- and low-grade migmatites and synkinematic emplacement of the Quiberon granite pluton. Quiberon is a well-known seaside resort and has some attractive beaches on the sheltered eastern coast.
Read more about Quiberon:
- Rapid Variscan exhumation and the role of magma in core complex formation: southern Brittany metamorphic belt, France
- Armorican Massiv Geological Map
- Quiberon peninsula
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