Originally composed by one single piece of rock, the Sidobre was cracked by the
Pyrenean orogeny, thus becoming more exposed to the
rhexistasy, which explain the remarkable natural forms and constructions of the site. The Sidobre, while just adjacent to it, is totally independent from the
Montagne Noire. They are separated by the
sedimentary basin of
Castres and the channel of the river
Thoré”. This stunning site, with its dozens of huge strange-shaped rocks, is unique in Europe (other sites exist in France, but in a much smaller scale), and has inspired many legends and tales. Image:Sidobre Peyro Clabado1.jpg|Le Peyro Clabado, on the commune of Lacrouzette Image:Sidobre Peyro Clabado2.jpg|Le Peyro Clabado Image:Sidobre Roc Oie.jpg|Le Roc de l'Oie (« The Rock of the Goose ») Image:Sidobre Saut Truite.jpg|Waterfall in the Sidobre Image:Rocher tremblant sept faux.jpg|Trembling rock in Sept-Faux ==Economy==