The Arsine corrie via the Crevasses path

17 points of interest

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  History

  Dismantled ski-lifts

  A small ski resort was created in 1970 not far from the Lautaret mountain pass. Due to the risk of avalanches and new standards required, alpine skiing was moved near to the village of Villar d'Arène and Chazelet hamlet. The two obsolete ski-lifts situated in this very   picturesque territory, rich in terms of biodiversity, ruin this place which has been classified since1974 as the national nature reserve of Combeynot. In 2013, dismantling was carried out by the Mixed union of ski-resorts in the Haute Romanche with the support of the National Park. In the end more than 35 tons of iron and concrete blocks were evacuated.

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  Flora

  Alder forest and green alders

  Here is a spectacular transition from the genuine forest and pastures of the north facing slopes. There is a thick grouping of shrubs made up essentially of willows and green alders. These will never reach the size of a tree. They constitute impenetrable thickets where, over time, boars, chamois and roe deer have outlined a maze to hide in. The plants provide nitrogen through their roots and fertilise the soil, as if getting their own back on the eutrophic tall herbs.
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  Flora

  Transition zone at the upper edge of the forest, it has large plants with big leaves that seek light in order to grow. Under cover of their leaves, some animals and plants find a safe haven, particularly alternate-leaved golden saxifrage and adenostyles alpina. On the east part of the Ecrins massif, eutrophic tall herbs can be found at the edge of streams and brooks. Just after snowmelt, it raises its golden head and constitutes a lovely carpet of flowers.
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  Flora

  Turk's cap lily

  The Turk's cap lily lodges on the grassy slopes, meadows and undergrowth. It can be seen from a distance due to it long upright flowering stalk from which stem three to ten majestic flowers. They are large, purple-pink with some crimson, and have six petals that turn upwards when they reach maturity. Six orange stamens are then visible. The flowers that bend downwards lift when the fruit is formed.
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  Fauna

  Black Grouse

  The black grouse lives above 1200 m, and can only be found in the Alps. It is possible to spot the male due to its black plumage and its tail in the shape of a lyre (which is why its French name is Tétras Lyre). While it spends most of the time in winter in an igloo scooped out of the snow as protection against the cold, in the spring it performs spectacular parades to attract a female. The National park is tracking the population of the species in this zone.
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  Glacier

  View over La Meije

  La Meije is the second major peak in the Massif des Ecrins. It is made up of 3 main peaks: the Doigt de Dieu (3,973 m), La Meije Orientale (3,891m), and the highest summit, the Grand Pic at 3,983 m. It is a hard summit to climb, and the first to do so, on 16 August 1877, was Emmanuel Boileau de Castelnau, together with the famous local guide, Pierre Gaspard. "Meije" comes from the Occitan word Meidjo, which means midday, because when seen from the village of La Grave, the sun passes above the summit at around noon. On the other side, before La Meije became famous, it was called the Bec des Peignes (“Comb Beak”) by the inhabitants of Saint-Christophe-en-Oisans.

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  Panorama

  Belvedere de l'homme

  A wooden guardrail is set up at the ideal spot for contemplating the descending glaciers of La Meije. The Lautaret glacier to the left and the Glacier de l’Homme to the right scarcely meet today. The last-named glacier is the descending ski slope from the Pic Oriental of La Meije and from the Aigle refuge (to be seen if you continue along the path towards the Rocher Blanc). The refuge is perched at an altitude of 3,450 m on a rocky spur. A new refuge was opened in 2014, preserving an existing wooden structure that dated from 1910.

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  Fauna

  The marmots’ "bosse"

  The alpine marmot is naturally present on grass at altitude. Here, it occupies a singular place which we call the marmots’  "bosse». This hibernating rodent is only visible between April and October. The marmot lives in a family and respects a hierarchy. Games, grooming, fighting and biting ensure the dominance of a couple as well as the cohesion of the group. Each animal participates in the delimitation of the territory by rubbing its cheeks on rocks and also by urinating and defecating there. When there is danger, the marmot emits a high and powerful whistle in order to warn the others.

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  Flora

  Felwort

  In early August, the felwort’s violet stars open in the sunshine. At the base of each of its five petals, two shiny pits full of nectar attract insects. A member of the gentian family, this beautiful flower is a perennial that survives the cold season with its persistent winter bud close to the ground, surrounded by a rosette of protecting leaves.

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  Pass

  Arsine pass

  The Arsine pass, is an important crossing point to visit on the GR54 Tour des Ecrins et de l'Oisans. It gives a remarkable viewpoint over the Angeaux massif. The pass is part of an old itinerary that was used instead of the crossing point by the Lautaret pass. It is also a crossing point between the Guisane and the Romanche area. This is an area that was mentioned as early as the Middle Ages as a place of conflict between the districts of Villar d'Arène and Monétier-les-Bains.
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  Flora

  Arctic rush

  Even though it is relatively common in some acidic marshland, the Arctic rush is nonetheless protected throughout the Rhône-Alpes and Provence-Alpes-Côte-d’Azur regions. It can be recognised because of its total absence of leaves and by the few blackish flowers in the upper third of the stalk. The flower tepals open at an obtuse angle and are a little shorter than the capsule.

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  Fauna

  Rock ptarmigan

  At five in the morning in the month of May, at an altitude of over 2,000 m, the sun rises over the fields of blueberry, which appear above the patches of snow. All of a sudden, a hoarse, almost metallic cry cuts through the peaceful dawn atmosphere: the rock ptarmigan is in the midst of its nuptial parade. Originating from the Arctic tundra, the rock ptarmigan, sometimes called the snow partridge, was to be found all over Europe during the ice ages, before its living space was limited to the mountains. Even today, it finds the conditions it needs to survive. The national Alpine parks have a great responsibility in conserving this species. The inventory carried out by the Haute-Romanche nature unit in 2005 showed there was a large core group of birds on the site.

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  Glacier

  Moraines

  The site of Arsine offers a complex moraine environment with a parade of ice margin flowers. The frontal moraine of the Arsine glacier is on a glacial vegetated rock complex that occupies about forty hectares at the bottom of the cirque. This complex is likely to have come about through a shifting of abandoned glacial deposits after permafrost was established. This means that the ground maintains a temperature of 0°C or less over several years. This phenomenon is likely to have taken place during the recent Dryas climatic cooling, that is to say 11 000 – 10 000 years BC.
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  Fauna

  Aquatic diet

  The grey wagtail is "hyperactive" and has a diet of flies, mosquitoes, dragonflies and all sorts of aquatic insect larvae. It hunts at the edge of the water, by jumping from stone to stone or hovers to catch its prey. It sometimes fishes for shellfish, molluscs, or even small fish to complete it meals. It does not leave the damp banks to build its nest either, and even looks for somewhere close to a waterfall or to flowing river.
     
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  Glacier

  Ice calving

  When the lake is frozen and the air temperature rises, the ice expands, provoking what is called the “song of the lake". The Lac Ouest is the last lake in the mountain range where it is still possible to see the fall of seracs (the front of the glacier) into the water, giving rise to this muffled noise.

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  Glacier

  The melting Arsine glacier

  Lake Arsine came to life in the 1950s after the Arsine glacier melted. Due to its rapid development, it was measured more accurately in 1969 and 1985, showing 800,000 m3 of water contained in a moraine that had been weakened by the ice inside it. Since it threatened to break, emergency work was undertaken the following spring to stop the rise in the level of the lake using a regulation channel dug across the frontal moraine. Almost 30 years later, the glacier site is still carefully monitored by Park employees. And the risk is now completely ruled out.

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  Lake

  Arsine Glacier

  The Arsine glacier is contained in the hollow of a vast corrie facing north, encircled by high walls reaching an altitude of between 3,200 and 3,600 metres. This is a glacier that is mostly hidden, with the front, currently at an altitude of about 2,470 m, behind lakes. The lakes are held back by an impressive series of old moraines, formed during the Little Ice Age (between about 1550 and 1850). Due to its size and preserved state, the old moraines of Arsine are an exception in the western Alps. Usually such morainic fronts are found in small, high-altitude glaciers, resulting water running too weakly to sweep away the accumulation of pre-glacier deposits (for example, the Réou d’Arsine glacier). The melting and shrinking of the Arsine glacier posed problems in the 1980s concerning water retention and therefore safety. RTM teams carried out work to lower the level of the lakes, the size of which raised fears of a break in the moraine with the risk of flooding the village of Le Casset.