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L'Alpe d'Huez (French pronunciation: [l‿al.pə d‿ɥɛz]) is a ski resort in Southeastern France at 1,250 to 3,330 metres (4,100 to 10,925 ft). It is a mountain pasture in the central French Western Alps, in the commune of Huez, which is part of the Isère department in the Auvergne-Rhône-Alpes region.
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The Alps event, being the more widely publicized and famous among downhill cycling enthusiasts, starts on the glaciated summit of Pic Blanc in Huez and descends to the valley bottom at Allemond, for a total of over 2,600 vertical meters (8530 feet) and a 20 km (12 miles) distance.
Huez (French pronunciation:) is a commune in the Isère department in southeastern France. The mountain resort Alpe d'Huez is located in the commune. L'Alpe d'Huez is often an ascent on the Tour de France .
A small chapel, built in 1940, situated in the center of the Alpe d'Huez, was initially dedicated to the Marian cult.In 1960, the priest, Jaap Reuten, asked Jean Le Boucher and architect Jean Marol to build a church-shaped tent, representing Abraham, the first Biblical patriarch, to replace the chapel with a structure visible from the Meije, in preparation for the Olympic Games of 1968.
From Alpe d'Huez, the route used on the Tour de France follows an unnamed road initially, descending to 1,765 m (5,791 ft) before the final climb to the summit which is 3 km (1.9 mi) long at an average gradient of 7.8%. [1] From the south, the road to the pass follows the D25 from its junction with the D1091 to the east of Le Freney-d'Oisans.
In the 2008 Tour, the Col du Galibier had been crossed on 23 July in the 210 km stage 17 from Embrun to Alpe d'Huez. [ 3 ] The 2011 Tour climbed the Col du Galibier twice to celebrate the 100th anniversary of the first appearance of the pass in the Tour de France, including the first ever summit finish, won by Andy Schleck after a 60 km solo ...
The snow line is measured using automatic cameras, aerial photographs, or satellite images. Because the snow line can be established without on-the-ground measurements, it can be measured in remote and difficult to access areas. Therefore, the snow line has become an important variable in hydrological models. [2]