20의 낭트가지 명소 & 주요 장소

taupe!

The rock formation covers approximately 120 hectares. It was formed by corrosion of the dolomite rock of the Causse Noir. It was originally assumed that the rocks were a ruined city, and it was not until 1870 that a trench was cut through the rocks. The speleologist Edouard-Alfred Martel was the first to map the rocks in 1883-1884.

The rock formation is located in the western part of the department on the high plateau of the Causse Noir. To the north lie the rivers Tarn and Jonte, to the south lie the Dourbie gorges, and to the west lies the town of Millau.

Long before the discovery of electricity and the associated inventions, our ancestors discovered the possibility of harnessing the power of the elements - which on the one hand were useful, but on the other hand could also be a threat as a force of nature - for various purposes. A suitable example of the human ingenuity of earlier generations is such a mill: the heavy millstones with which, for example, grain was ground into grain or oil was pressed, could be powered with the help of water or - as here - the wind. Hardly any of them still fulfill their original functions today, but fortunately some have at least been preserved as evidence of the old days.

Please wear sturdy clothing that can get dirty/wet. There are climbing passages - a light summer dress is not suitable.

The Rédounel windmill is one of the first mills on the Larzac causses. It accompanied the agricultural activities of the Templars established in La Couvertoirade from the 12th century. It has been restored and is still in remarkable condition today.

The Roc Nantais is a rock in the shape of a monumental tower dominating the Dourbie at 808m. It obviously offers a magnificent viewpoint from which to admire the Larzac and the foothills of the Cévennes (on the left), the St-Alban (opposite) and the Causse des Cuns (on the right).

The canoles are impressive faults dug by the erosion of the limestone. If the site is today an ideal place for hiking, it has been a habitat since the Mesolithic.