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Pelite

Pélites rouges des gorges de Daluis.
Credit : Eric LE BOUTEILLER

Description

It was at the end of the primary era and the Permian era 250 million years ago that these vast red lands were born. The erosion of a very ancient crystalline mountain range led to fine silt mixed with volcanic ash being deposited on a flood plain. Pressure and heat transformed this accumulation of sediment into pelite. Their red-wine colour is the result of oxidation of the iron that they contain. Nine hundred metres of deposits are visible below Cime du Barrot.

Technical Information

Lat, Lng
44.06200956.8630504
Coordinates copied
Uncertain state
Point of Interest updated on 01/01/1970
This point of interest hasn't been updated recently, which could compromise the reliability of this information. We recommend that you inquire and take all necessary precautions. If you're the author, please verify your information.

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! 🌳🥾