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Cargneule

Cargneule
Credit : ©Jean-Baptiste Portier - PNR Queyras

Description

Landmark 11The rocky peaks overlooking you are made of a special vacuolar rock: the cargneule. These cells (or "holes") are formed by the melting of the dolomite constituting the initial rock. This melting is due to acidified waters by the dissolution of gypsum in the immediate vicinity. Since the appearance of these cavities, today, the rainwater continues the erosive work and facilitate the creation of caves: the "balmes" or the "balms".

Technical Information

Lat, Lng
44.84806716.7340507
Coordinates copied
Point of Interest updated on 30/11/2025

Altimetric profile

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Caution!
We have no information on the difficulty of this circuit. You may encounter some surprises along the way. Before you go, please feel free to inquire more and take all necessary precautions. Have a good trip! 🌳🥾