Showing posts with label Geotourism. Show all posts
Showing posts with label Geotourism. Show all posts

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

Tuesday, February 10, 2009

Rhine Falls.

Glaciation and warm interglacial periods of the past 500'000 years have shaped the landscape from the high rising Alps down to the northern lowlands of Switzerland. In the area of Schaffhausen the river Rhine has changed its course several times eroding Jurassic limestone and filling channels with gravel and sand. At the location of the famous Rhine waterfall the present-day river bed consists at the upper side of hard Jurassic (150 million years old) limestones which terminate in a cliff bordering gravel beds of an abandoned river channel formed by the ancient Rhine during Riss age (about 120'000 years old). The waterfall developped about 15'000 years ago, after the new Rhine started to erode the soft Riss-age gravel and sands.
Literature:
Albert Heim, 1931, Geologie des Rheinfalls.
Der Rheinfall, Neujahrsblatt der Naturforschenden Gesellschaft Schaffhausen, Nr. 39, 1987.
http://www.knill.com/Rheinfall/Wissen/Geologie.html
http://www.rua.ch/rhein/Region03Destination01Entstehung.htm



The Rhine Falls are the largest waterfalls in Europe.
Latitude: 47.677871
Longitude: 8.614482
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Panoramio
Photo Stadtarchiv Schaffhausen

Wednesday, January 14, 2009

Volcanism at Jaujac, Ardèche, France

Outcrops of a young volcano at Jaujac village and the lava rocks are unique in the world and excite geologists and most other people.

The lava of a very young volcano has spread over the ancient river bed seen at the base of the basalt columns.

Read more about it.

Tuesday, January 13, 2009

Pont d'Arc


Pont d'Arc - Wikipedia: "The Pont d'Arc (French pont = bridge) is a great natural bridge, located in the Ardèche département in the south of France, near the town of Vallon-Pont-d'Arc.

The bridge has a width of 60 m and a height of 45 m and was carved out by the Ardèche River."
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