Generated by DeepSeek V3.2| Pointe de Charbonnel | |
|---|---|
| Name | Pointe de Charbonnel |
| Photo caption | View of the Mont Cenis massif, with Pointe de Charbonnel prominent. |
| Elevation m | 3752 |
| Prominence m | 1502 |
| Listing | Alpine 3000er |
| Location | Savoie, France / Piedmont, Italy |
| Range | Graian Alps / Mont Cenis massif |
| Coordinates | 45, 16, 42, N... |
| First ascent | 10 August 1862 by Michel Croz with party |
| Easiest route | Glacier/snow climb |
Pointe de Charbonnel is a prominent mountain summit in the Graian Alps, forming the highest point of the Mont Cenis massif on the border between France and Italy. With an elevation of 3,752 meters, it is a major peak in the Vanoise region and a notable feature of the Arc river valley skyline. Its imposing north face overlooks the Maurienne valley, while its southern slopes descend into the Italian Cenischia valley.
Pointe de Charbonnel is situated on the watershed between the French Alps and the Italian Alps, precisely on the border of the Savoie department in France and the Metropolitan City of Turin in the Piedmont region of Italy. The mountain anchors the western end of the Mont Cenis plateau, a historically significant alpine pass region. Major nearby peaks include Aiguille de Scolette and Grand Roc Noir, while the summit provides extensive views of the Écrins massif, Mont Blanc, and the Gran Paradiso. Key valleys radiating from it include the Maurienne, the Haute-Maurienne, and the Val Cenischia, with the Arc and Dora Riparia rivers originating on its flanks.
The mountain is primarily composed of metamorphic rocks, specifically gneiss and micaschist, which are characteristic of the Briançonnais geologic zone within the broader Alpine orogeny. Its structure was shaped by the tectonic collision between the Apulian Plate and the Eurasian Plate, with significant uplift and folding occurring during the Tertiary period. The distinct, sharp summit ridge and steep northern face are the result of extensive Quaternary glaciation, primarily from the Würm glaciation, which carved out the surrounding cirques like the Vallon de l'Arc and left behind several remnant glaciers, including the Glacier de Charbonnel.
The first recorded ascent was achieved on 10 August 1862 by the famed Chamonix guide Michel Croz, along with Felix and Henry Devouassoud and J. A. G. Marshall. The standard route, the **Normal Route**, approaches from the Italian side via the Rifugio Avanzà or the Rifugio Levi Molinari, involving glacier travel on the Ghiacciaio di Sea and a mixed rock and snow ridge. From the French side, ascents typically start from Bonneval-sur-Arc or Lanslebourg-Mont-Cenis, requiring traversal of the Glacier de Charbonnel. The climb is graded **PD/AD** on the Alpine grading system and is considered a classic high-altitude glacier route, often included in traverses of the Mont Cenis range. The nearby Col du Mont Cenis provides major road access to the region.
The area around Pointe de Charbonnel has been a strategic crossroads since antiquity, with the Mont Cenis pass used by Hannibal, Charlemagne, and Napoleon Bonaparte for military campaigns. The mountain itself remained unclimbed until the Golden Age of Alpinism, with Croz's ascent following the first ascents of nearby peaks like the Grandes Jorasses. The region saw significant fortification in the late 19th and early 20th centuries as part of the Alpine Line and Vallo Alpino defenses between France and Italy. The construction of the Fréjus Rail Tunnel and the Mont Cenis dam in the 19th century increased accessibility, drawing early Club Alpin Français and Club Alpino Italiano explorers to its slopes.
The mountain's altitudinal zones support diverse habitats within the Vanoise National Park on the French side and the contiguous Gran Paradiso National Park in Italy. Lower slopes are characterized by Alpine grassland and larch forests, giving way to alpine meadows hosting species like Rhododendron ferrugineum and Gentiana acaulis. The high alpine zone is a habitat for Alpine chamois, Alpine marmot, and the elusive rock ptarmigan. The remnant glaciers are important indicators of climate change, having receded significantly since the Little Ice Age. The area is part of the Natura 2000 network and is managed for conservation, with research conducted by the University of Savoy and the University of Turin on alpine flora and glacial retreat.
Category:Mountains of Savoie Category:Mountains of Piedmont Category:Alpine three-thousanders Category:International mountains of Europe Category:Mont Cenis