The communal eucalyptus forest is located northwest of the village of Cessenon on the D14. In 1958, an experimental plantation of a dozen species of eucalyptus over an area of 14 ha replaced the maquis. In 1984, all eucalyptus froze. The suckers then form a forest thicket next to 25 ha of maritime pines. A marked hiking trail Read more...
In the heart of the Haut-Languedoc regional natural park, the cave is nicknamed the “Palace of the Glass Spinner” for the beauty and finesse of its various shapes. The work of water has sculpted a profusion of forms: stalactites, stalagmites, aragonite flowers. One and only cave in the Haut Languedoc Natural Park, classified site, Label Vélo and Natura 2000! Read more...
Part of the commune of Assignan is classified as a Natura 2000 zone: a marbled newt permanently inhabits the communal pond which is never dried up. Walkers can see this greenish-colored ocellated lizard warming up in the sun, during a walk on the Barralets trail. Read more...
A long time ago, the sea arrived at the foot of the village of Capestang, whose name means “Cape of the pond”. Thanks to its salt pans, the Capestang pond was, from the early Middle Ages, an important source of income for the region which the archbishops of Narbonne would not fail to exploit. The Etang de Capestang is a wetland Read more...
Of very high quality, marble has been used to decorate prestigious buildings such as the White House in Washington or the House of France in Rio de Janeiro. On the geological aspect, the recording of the crisis characterizing the end of the primary era is particularly remarkable within the layers which outcrop in the Coumiac quarry, which is why this Read more...
A magnificent corner of nature in southern Hérault, near Cessenon-sur-Orb At a place called Réals, a dolomitic chaos where the rock forms deep gorges, the Orb rushes into a passage forming impressive rapids. A little further on is the Pont de Réals, a beautiful work from the end of the 19th century, it has 5 vaults of 13 meters on the Read more...
The rocky bars of Cazedarnes constitute a limestone layer deposited in a lake 65 million years ago, then folded under the effect of the appearance of the Pyrenees. Erosion ended up digging valleys between the bars that remained in relief. Read more...
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