GTN CycleTours |
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Tour du Vercors Nord
The PréAlpes were formed in the Secondary Era from about 200 to 65 million years ago, when there was a sea where the Alps now stand. The Alps are where the European and African plates of the Earth's crust meet and were crumpled up in the Tertiary Era (65 to 2 million years ago) under pressure from the Italian side. The Vercors is encircled by a mountainous ridge at up to two thousand metres high within three rivers - the Rhône to the west, the Isère to the north and the Drôme to the south - making the Vercors an easily defended natural fortress with only a handful of entrances. Throughout history the occupants have asserted their opposition to outside oppression - whether medieval warlords refusing the King or the French Resistance opposing the German invasion during the Second World War. There are two narrow and steep ways into the Vercors from the north: through the Gorge of the river Furon or the 1100 metre crossing of the end of the Montagne de Lans ridge to the head of the Bourne valley. There is also the Tunnel du Mortier at the top of the Meaudret valley but the road is permanently blocked by a landslide on the north side. The 2000 metre high Montagne de Lans ridge forms a natural barrier to any easy access to the Vercors from the east. ![]()
The three river valleys within the Vercors - the Bourne, the Meaudret and the Vernaison - are at 800 to 1000 metres and run north or south until they all turn west and meet at the Bourne gorge. The Bourne river is the only way out for the Vercors rain, which ends up in the Isère river to the west and, via the Rhone river, in the Mediterranean at the Camargue region near Marseille. Limestone uplands like the Vercors usually have extensive caves formed from water erosion by the underground rivers, and many are accessible. The Vercors is renowned for its caves and the best known is the Gouffre Berger which held the deepest underground exploration record of 1200m for many years. |
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