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Faille de Ser Barbier

Description

La faille de Ser Barbier met en contact un socle cristallin (aiguille de Venosc) et un dépôt marneux (col du Vallon). Elle s'est formée au jurassique lors de l'ouverture de la mer Téthys, par cassure et effondrement du massif cristallin. Le frottement des deux parties a créé un beau miroir strié bien dégagé par l'érosion.

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Lat, Lng
44.95670116.0966272
Coordinates copied
Point of Interest updated on 18/11/2025

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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! 🌳🥾