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Chamonix-Mont-Blanc (French pronunciation: [ʃamɔni mɔ̃ blɑ̃]; Arpitan: Chamôni-Mont-Blanc), more commonly known simply as Chamonix (Chamôni), [a] [b] is a commune in the Haute-Savoie department in the Auvergne-Rhône-Alpes region in Southeastern France. It was the site of the first Winter Olympics, held in 1924.
There are two sections: from Chamonix to Plan de l'Aiguille at 2,317 m (7,602 ft) and then directly, without any support pillar, to the upper station at 3,777 m (the building contains an elevator to the summit). The span of the second section is 2,867 m (1.781 mi) measured directly, but only 2,500 m (1.6 mi) measured horizontally.
The France–Italy border is mainly mountainous. It is 515 kilometres (320 mi) long, [1] in southeast France and northwest Italy. It begins at the west tripoint of France–Italy–Switzerland near the top of Mont Dolent (3,820 m), in the French commune of Chamonix (department of Haute-Savoie), the Italian city of Courmayeur (Aosta Valley) and the Swiss commune of Orsières (canton of Valais
The Aiguille du Midi Cable Car in Chamonix attracts 500,000 people each year and gives views over much of the massif, and up towards Mont Blanc itself. From Chamonix it rises to the summit of the Aiguille du Midi at 3,842 metres (12,605 ft), and holds the world record for the highest vertical ascent of any cable car (2,807 m (9,209 ft)). [5]
Argentière is located near the head of the Valley of Chamonix approximately 7 km (4 mi) from Chamonix town. It is connected by road with Switzerland by the pass over the Col des Montets and the Col de la Forclaz to Martigny in the Rhône Valley.
The French Alps (French: Alpes françaises; Arpitan: Ârpes francêses; Occitan: Aups francesas; Ligurian: Arpi françéixi) are the portions of the Alps mountain range that stand within France, located in the Auvergne-Rhône-Alpes and Provence-Alpes-Côte d'Azur regions.
The glacier lies above the Chamonix valley. The pressure within the ice is known to reach at least 30 atmospheres. [3] The Mer de Glace can be considered as originating at an elevation of 2,100 metres (6,900 ft), just north of the Aiguille du Tacul, where it is formed by the confluence of the Glacier de Leschaux and the Glacier du Tacul.
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