From valley to valley – between Gardon and Tarnon (day 2)

8 points of interest

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  History

  The age of silk

  From the 19th century onwards, the silk industry developed in the Cévennes: tanneries gave way to spinning mills. The mills used water not only to treat the silkworm cocoons (which were boiled to prepare the silk) but also for the steam-driven spinning machines. In the second half of the 19th century, diseases strongly reduced silk production, which was also subject to competition from foreign silks and then from artificial silk. The silk industry went under in 1965.

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  History

  The tanners’ district

  La Calquière district gets its name from that of the ditches in which the tanners soaked their animal skins with limestone, which is called cauç or calç in Occitan. All along the Gardon there were tanneries because its acidic water was good for rinsing the skins, which was indispensable for obtaining high quality products.

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  History

  Lique Ser

  Lique Ser path goes up to the famous Corniche des Cévennes, a ridge between the two departments of Gard and Lozère. This road, which is busy these days in summer because of its superb views, has not always been a holiday address.
  In the days of Louis XIII and XIV, this was the route of the dragonnades and the repression of Protestantism by the King’s army after the Revocation of the Edict (the billeting of deliberately ill-disciplined soldiers in Protestant households) of Nantes. This ridge gave the soldiers, known as the King’s dragoons, strategic viewpoints. The road was abandoned from the 19th century onwards. In 1930, after lengthy renovations, it was opened to traffic again, becoming a major tourist route

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  History

  Le Pompidou

  Le Pompidou, like Saint-Roman de Tousque, owes its development to its location on the Corniche des Cévennes road. From the 17th century onwards, this former mule track carried substantial trade, with mule cart drivers bringing up salt, wine and dried fish from southern France to the Gévaudan, taking grains and cloth down from the uplands, and exporting the silk and chestnuts of the Cévennes. You can still see two buildings, the former inn (Le Cheval Blanc) and the Chapeau Rouge staging post, where travellers changed carriage horses.

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  Agriculture

  Small buildings

  The small buildings you see dotted here and there are jasses (from jas: place where livestock sleeps), sheepfolds of times gone by. There used to be at least 20 between Tartabissac and Bézuc. From the first warm days to 6 December, livestock would spend the night here, and their owners would come up during the day to watch them. An old saying goes, “No livestock in the chestnut groves before the sixth of December”. 6 December was the date of the fair in Florac when the local chestnuts were sold. Today Bézuc hosts 200 sheep for 8 months of the year.

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  Geology

  Contact

  At the Col de Tartabisac pass, there is a clear limit between the two bedrocks: on the left, the limestone plateau; on the right, a schist slope. The two rocks are in contact at a geological fault. A layer of very wet sandstone sits at the level of the meadows, at the foot of the limestone. This is where the water that has infiltrated via the thick layers of the Can plateau re-emerges. 

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  Geology

  Schist, limestone or granite

  From the track, you can make out the hamlets on the side of the valley at the foot of the Can: Roumassel, Le Crouzet, Le Crémat, Le Masbonnet. The land stretching from the valley floor to the plateau belongs to these hamlets, including chestnut groves, pasture and parcels for growing grains. After Bézuc, the bedrock is partly schist, where broom and heather grow, partly limestone, which is linked to the presence of the carline thistle. In a meadow beyond the beech forest, you can see blocks of granite, which stem from a vein linking Mont Aigoual to Mont Lozère. The ruiniform rocks on the plateau were shaped by water, which infiltrates fractures in the rock and dissolves the dolomite that they are made of.

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  Flora

  Ash trees

  Ash trees, like the ones that border the path, like cool and damp environments. They were planted alongside paths by locals because ash branches, cut towards the end of summer, provided additional fodder for livestock.