Gorges du Tarn
The Gorges du Tarn is a canyon formed by the Tarn River between the Causse Méjean and the Causse de Sauveterre, in southern France. The canyon, mainly located in the Lozère département, and partially in the Aveyron département, is about 53 kilometres (33 mi)-long (from the village of Quézac to Le Rozier, from to Coordinates: ) and 400m to 600m deep.
The architecture of the gorges involves mesozoic limestone plateaux downstream presenting sub-vertical cliffs. Faults like the Hauterive Fault upstream explain the important water sources in the region of Saint-Enimie (the Burle source and the Coussac source, the latter joining the Tarn in an impressive waterfall), and the more complex geology.
In the quaternary, the gorges were also affected by a volcanic activity whose traces can be found in the Sauveterre Causse, in the form of a double volcanic dip, and in the basaltic rocks next to Eglanzines.
The climate is mediterranean, with relatively mild winters and very warm summers.
Tourism is a main factor of development in the region, with activities that include :
- Speleology in the Causses
- Visiting typical villages : Cirque de Saint-Chély-du-Tarn, ...
- Rock climbing
- Outdoor sports and leisures...
|Wikimedia Commons has media related to Gorges du Tarn.|
|This article related to geography of France is a stub. You can help Wikipedia by expanding it.|