4. Tour of Vieux Chaillol - Stage 4 out of 5

9 points of interest

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  History

  Les Borels

  This is most important village in the Chamoléon district (no hamlet bears this name). Until towards the first world war in 1914, the valley lived in a closed circuit for all everyday items. At the Borels there was a weaver (wool and hemp), a miller-baker, an ironmonger, a mason, a breeches-maker and in the other hamlets, a cobbler, two millers, a joiner and two shoemakers. The latter worked from home.
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  Fauna

  Alpine ibex

  If you take a few minutes' walk at the end of the valley, you will be able to see some Alpine ibex. In September 1994, in Champoléon, some thirty animals from Vanoise area were released by Ecrins National Park rangers. This superb animal is heavier (100 kg) and less timid than the chamois, and is closely related to the domestic goat. It was almost extinct in the Alps. Today it is totally protected in France and is now safe extinction.

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  History

  Champoleon

  To the 24 questions asked by the attorney general of the Dauphiné in 1789, the Champoléon Council replied, "Champoléon is in the most atrocious place of the Haut-Dauphiné. The community has 16 villages, 80 families and 600 souls spread over the slopes of the mountain. All of the roofs are thatched [...] the rivers and streams cause serious damage." Indeed, on All Saints Day in 1790, the Champoléon church was destroyed by flooding. Part of the graveyard was washed away taking coffins and corpses away from Champoléon too.
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  Geology and geography

  Geology

  Upstream from Les Borels, the right-hand side of Champoléon is dominated by peaks without stratification, made up of crystalline rocks (granite and gneiss). They are protruding and pushing back the older, softer sedimentary rocks found on the other side (limestone and sandstone). These movements have caused faults and mineralisation which was exploited in past times (pyrite, galena, copper…) 

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  Vernacular heritage

  Les Richards

  Perched up at an altitude of 1548 m above Pont-du-Fossé in the commune of Saint-Jean-Saint-Nicolas, the village of Les Richards is a haven of tranquillity. The view is breathtaking over the Autanes and the Champsaur woodlands. This is the starting point for a very popular hiking trail around the mountains or to the summit of the Palastre, and a take-off area for long-distance hang-gliders. It is not unusual for a hang-glider to land in Grenoble and sometimes even in Chamonix after a long day's flight from Les Richards! The record is 162 km, with a landing in Chamonix in 2002. 

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  Fauna

  Short-toed snake eagle

  This bird of prey can be recognised because of its large head, its quite impressive wingspan (1.80m) and the white plumage under its wings and body. Despite its size, it rarely eat small mammals. Its food mainly consists of lizards and snakes. When it hunts, it takes up a particular position against the wind, poised in the air with its wings fully outstretched.

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  Vernacular heritage

  Les Roranches Chapel

  Built in 1780 on the site of a former chapel dedicated to Our Lady of the Assumption, the Roranches chapel is dedicated to Saint Pancras, the protector of farm animals and pets. It was built using humble architectural techniques, and is highly representative of the small places of worship in the Champsaur woodlands where, as so often in the mountains, the materials used were those that were ready to hand. Two renovation projects have been carried out on the chapel since 2013 with the support of the Ecrins National Park. The first was aimed at stabilising the barrel vault and renewing the framework and roof using the original material, slate. The second project was to restore the plasterwork inside and outside, as well as the whitewash, windows and flooring.

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  Flora

  Scots pine

  The Scots pine can be recognised by its long reddish brown trunk and sparse foliage. The needles are grey-green, slightly curved and paired. It needs a great deal of sunshine, but can make do with poor, sandy soil that is unsuited to other trees. Its wood is light and of high quality.

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  Geology and geography

  Le Vieux Chaillol

  Easily visible from Champsaur and from beyond Gap, Le Vieux Chaillol is, like the Ecrins range, made up of granite rocks originating in the bedrock of the Cambrian era and which suddenly rose up some 5 million years ago. But the rocks of Le Vieux Chaillol have undergone a particular recrystallisation and have been transformed into metamorphic conglomerates and schists.