|Location:||Grottes et Cascade de Villecroze, Gorges du Verdon. 8km from Aups and 24km from Bauduen. 15km west of Draguignan on the D557, or 40km south of Moustiers-Ste-Marie (D957) and 8km southeast of Aups on the D557.|
Park: All year daily during daylight hours.
Caves: MAY to SEP daily.
Adults EUR 2.
|Classification:||Tufa cave Primary cave|
|Photography:||Allowed, but no flash.|
|Accessibility:||No, many stairs|
Information: Mairie, Tel: +33-494-706306, Fax: +33-494-675329.
Villecroze Tourist Office, 83690 Villecroze, Tel: +33-494-675000, Fax: +33-494-706750.
|As far as we know this information was accurate when it was published (see years in brackets), but may have changed since then.
Please check rates and details directly with the companies in question if you need more recent info.
|Prehistoric||this is a Neolithic site, and there are many finds in the local museum.|
|1065||first reference, Castrum de villa Crosa.|
|1566||caves fortified by Nicolas d'Albertas.|
|1633||ownership of the caves ceded to the commune of Villecroze.|
The town Villecroze is located in a flat and fertile valley, at the foot of barren limestone hill. At the far end of the village, below the limestone cliffs, lies a strange and romantic place named Parc Floral Municipal. This beautiful spot with nicely shaped plants, trails and benches, is a municipal park which could be found in many villages. But the white cliffs at the northern side are exceptional.
The cliffs contain numerous caves, named Grottes Troglodytes which means cave-dwellers caves - obviously a tautology, or at least a pleonasm. The cliffs consist of travertine, also named sweetwater limestone or tufa, which is limestone deposited by limestone rich karst water when it reaches the surface and looses its carbon dioxide content rather fast. The carbon dioxide was responsible for the ability of the water to dissolve limstone, without it the limstone crystallizes. Because of plant growth (which adds to the carbon dioxide consuption) the limstone is rather porous. The plants are covered by limstone crusts, then die and decompose, leaving an opening in the limestone. This is easy to see at the porous limestone cliffs.
A 40m high waterfall cascades down the front of the cliffs on the left side. This is the water responsible for the formation of the tufa deposit. The deposit is rather young, in geologic terms, but not recent. It was formed 700,000 years ago, when probably much more water was flowing down the brook forming a series of waterfalls.
High in the cliffs are a group of natural caves, which were formed by the irregular growth of the limestone. Some of those caves were transformed into dwellings, cave houses, which overlook the medieval village. This happened during the Middle Ages. The local Lord, Nicolas d'Albertas, decided in 1566 to built a fortification into the natural caves. They had enormous strategic benefits, it was only necessary to defend the front side, as the rest was surrounded by massive rock. And the rock was soft enough to make the construction much easier. The rock hewn out to create passages was immediatly used to build walls and staircases. However, nothing happened and the town was never under attack or besieged. The fortification were thus never needed, and after many years - in 1633 - Nicolas d'Albertas ceded ownership of the caves to the commune of Villecroze.
The front room are formed by closing overhanging cliffs with walls, and are lighted from windows facing out across to the village. Arched openings with staircases lead into the natural caves behind, which show the typical structures of the tufa and also many stalactites and other speleothems.
The caves are entered throuh a door on the left side of the terrace with the walls. Inside is a large room where the ticket seller explains the caves in French and English.