Chambeyron massif explained

Chambeyron Massif
Map:France Provence-Alpes-Côte d'Azur#France#Italy Piedmont#Italy
Age:Cretaceous to Pre-Permian
Parent Peak:Aiguille de Chambeyron
Elevation M:3412

The Chambeyron massif are a massif in the Alps, straddling between France and Italy, between the Escreins massif, the Cottian Alps and the Mercantour-Argentera massif. It occupies the high valleys of Ubaye, Maira, Varaita and Stura di Demonte.[1]

Main summits

The main peaks are:

Geology

The massif is part of the Internal Alps and it is mainly made up of sedimentary rocks, notably dolomitic limestones and shale.[2]

Glaciation

The Chambeyron massif is very lightly glaciated. Most glaciers are disappearing, or have disappeared during the 20th century. Only the Marinet glaciers (north face of the Aiguille de Chambeyron), as well as the Chauvet glacier, remain.[3]

Notes and References

  1. Book: Bulletin de la Société géologique de France . 1957 . La Société . fr.
  2. Web site: Haute vallée de l'Ubaye - Massif de Chambeyron - Rochers de Saint-Ours - Tête de Moïse . 2024-06-03 . Inventaire National du Patrimoine Naturel . fr.
  3. Book: Griselin, Madeleine . 3e symposium international, cavités glaciaires et cryokarst en régions polaires et de haute montagne: Chamonix-France, 1er-6 novembre 1994 : actes . 1995 . Presses Univ. Franche-Comté . 978-2-251-60561-6 . fr.