The White Glacier

The White Glacier

History and architecture
Lake and glacier
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A hike to come in to contact with the white glacier and to approach the mythical summits conquered by the mountaineers of the 19th century. 

"I started my career as park ranger in Valgaudemar before joining the Vallouise in 1982. I remember my astonishment when, climbing the white glacier, I saw the immense wall of ice that overhung the walkway... In my memories, ten years ago, the glacial front ended upwind. Interested by this progression, I started to take measurements, helped by my colleagues, in order to follow its evolution.  From 1986, the glacier has entered a recessive phase."

Joël Faure, park ranger. 


From the chalet-hôtel, go up towards the North-East to cross the walkways across the Momie torrents and the Black Glacier. The path goes up next to join the little mounds of smooth rock, worn and polished.

  1. The path crosses the bifurcation of the Black Glacier itinerary (which goes off to the left). Next, follow the bends.
  2. Cross the walkway across the White Glacier torrent, the path then follows the left bank of the torrent then goes right up to the ancient Tuckett refuge. Follow the slope to get to the White Glacier refuge and the Ecrins.
  3. Retrace your steps to descend to Pré de Madame Carle. 
  • Departure : Pré de Madame Carle, Pelvoux
  • Towns crossed : Vallouise-Pelvoux

12 points of interest

  • Geology and geography

    Weaving torrents

    A constantly changing environment, the weaving torrents are formed from the ancient remains of a glacial lake. They are made of interlaced lakes with arms of water that fluctuate depending on level of flood water in a zone where the slope because suddenly very gentle... Materials carried by the torrents over the steep slopes are deposited here creating islets which are eroded and built up again in time. These natural habitats which are rare and fragile shelter unusual plants. The weaving torrents give an unusual character to the landscape at the bottom of the glacial valleys. Their aspect is greatly enhanced when seen from the surrounding summits and glacial cross cliffs.

  • Glacier

    The Glacial valley

    The particularity of this valley is that it shelters both a white glacier which stays covered with ice and a black glacier composed of ice covered with rocks...  Their glacial tongues fluctuate depending on climatic conditions, which greatly effects the shape of the landscape. A lithography dating from 1854 shows the two glaciers joined at Pré de Madame Carle, ten years before the first ascent of the Barre des Ecrins. They white glacier lost more than 2 kilometers in length between 1885 and the 2000s.

  • Flora

    Rock clover

    Tiny clover dominates the alluvions or moraines in continual movement; the rock clover reproduces from seed each year unlike other alpine plants which are generally perennial. This strategy enables it to colonize areas which are always changing. It is a rare species protected nationally.

  • History

    The Barre des Ecrins

    The Barre des Ecrins (at an altitude of 4 102m , situated in the  direction of the Black Glacier) was climbed for the first time in 1864, from the North side, by Edouard Whymper accompanied  by Moore, Walker as well as his guides Almer and Michel. The Southern slope, was climbed for the first time by Henri Duhamel in 1880, with his guides Pierre Gaspard father and son from Bérarde. Then then came the time of a search for increasingly more difficult routes, In 1893, Auguste Reynier with his guides Joseph Turc and Maximin Gaspard, opened the way which now carries his name on the South-East face. The Southern column was opened in 1944 by Jeanne and Jean Franco.

  • Top

    The highest summit in the Ecrins

    On the borders of the Isère and the Hautes-Alpes, little known and once called the "pointe des Arsines", the Barre des Ecrins was once misnamed by the cartographers. So the Pelvoux was considered to be the highest point in the region and also in France at a time when the Savoie was independent. Also when in 1828 Capitaine Durand, a cartographer, made the first ascent of Pelvoux he was convinced that the status of the highest summit should be attributed to the Barre des Ecrins (4 102m).

  • Glacier

    The White Glacier and movement

    The White glacier has been monitored for a century. At the end of the 19th century, the White glacier Blanc joined the Black glacier at the Pré de Madame Carle. The path following the right bank and the moraine and crosses under the White glacier refuge. During the 20th century, the two glaciers constantly recede. This glacial decline was interspersed with advances with a spectacular one in the 1980s. Two markers of these impressive movements are the measures of the speed of the flow by posts as well as the scale put in place at the beginning of the 1980s. The debate concerning this operation has started again. should it be continued, should it be preserved ? The scale, which was no longer usable became dangerous, and was finally dismantled in 2008 because the old itinerary has been freed from ice and can now be used... One part has been preserved at the house of the mountains at Ailefroide. While we speak of eternal snows, the glacier fluctuates according to the changes in climate.

  • Fauna

    Yellow billed Chough

    A great diver and acrobat in the mountain tops, the yellow billed chough is also very clever at gleaning the remains of hikers’ picnics. It mainly moves in groups and brightens its passage with little fluted cries which are easily recognizable. It is as much a companion to experienced mountaineers as those just out for the day.

  • Fauna

    Alpine Accentor

    The Alpine Accentor, is more discreet that the Yellow billed Chough, the same size as a sparrow is another inhabitant of these altitudes. It is never far away... On the top a few black stripes decorate its ash coloured feathers. Red flames characteristically mark its flanks  It trots on the short grass in the alpine prairies and crows on the bare stone. It comes to peck the crumbs around the refuge. When winter comes it migrates towards the vallies. This transhumance even extends to the rocks of the littoral. When the snow melts, along the banks of snow, It is an impressive predator catching the small invertebrates numbed by the cold.

  • Glacier

    Life on the White Glacier

    Life nestles everywhere. There is no exception !  Unicellular algae are capable of developing on the surface of the snow giving the snow banks a pink coloration. The animal world is represented by the springtail (collembole), a primitive insect that measures between 1 and 2 mm, and which lives in little pools in the ice. It feeds on little nutritive particles carried by the wind. Its development takes place between 0 and 4°c. As soon as the temperature reaches 12°C, it burrows down in order to satisfy its thermic requirement indispensable for its survival... Sometimes other animals adventure out putting their lives in danger.

  • Glacier

    Glacier monitoring

    Each year, the Ecrins National Park makes photographic records, mass balances, monitors the glacial front and takes topographical measurements. In the context of precocious evolution of the climate, it is an important program in the domain of high European mountains.

  • Hut

    Tuckett Refuge

    The refuge is an ancient witness to the pioneering days of mountaineering in Vallouise in the second half of the 19th century... At that time it was situated at the foot of the glacier. It was built in 1886 to provide shelter under the rock for the first mountaineers. With its small dimensions, and materials of stone and wood, it represents a historical reference. Its remains shelter an exhibition retracing its history.

  • Glacier

    Evolution of the glaciers

    The glacier symbolizes the evolution of the climate through the ages: it only seems to be immobile. It is the relative size of the accumulation of snow in winter in the upper part of the  glacier and the amount of ice melting in the lower part of the glacier in the summer that determine the progression or the retreat of the glacier. Since the 1990s, under the probable effect of global warming with warmer summers and less snow winters, the glaciers retreat more strongly. Concerning the flow of the glacier, a snowflake that falls at the summit of the dome will take around a century to reach the front of glacier. Transformed into a drop of water, it will join the glacial torrent...


Altimetric profile


Summer itinerary: check that the access road to Pré de Madame Carle is open and that the walkways have been put back in place across the torrents... Payment has been required since 2013 at the communal car park at Pré de Madame Carle.

Is in the midst of the park
The national park is an unrestricted natural area but subjected to regulations which must be known by all visitors.

Information desks

Information center Pré de Mme Carle (summer only)

Pré de Madame Carle, 05340 Pelvoux

Information, documentation and exhibition on glaciers, sale of products and works of the Park. Occasional wildlife sightings to the telescope. Free admission. All animations of the Park are free unless otherwise stated.

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Coach stop : Pré Madame Carle

Access and parking

At  23 km from l'Argentière-la-Bessée on the D994E, reach Vallouise. Then cross Pelvoux, Ailefroide and take the D204T until Pré de Madame Carle. 

More information


Parc national des Ecrins

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