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Chamoson belongs to a geological region characterized by large outcrops
of limestone, shale and slate covering the European continental basement,
itself composed of granite and gneiss.
The vineyards of Chamoson sit on three distinct geological formations
with widely different soils and forms:
A)
The massifs and peaks (Ardévaz, Haut-de-Cry, Dent de Chamosentze,
Grand Muveran, etc.)
surrounding Chamoson are composed of sedimentary rock of marine
origin deposited on continental Europe’s crystalline basement.
B) Glacial and moraine deposits
dating from the last glacial period of the Quaternary (about
10,000 BP) were left by local glaciers that developed on the eroded remains
of the massive Rhodanian glacier as it retreated from what is now the
Rhône Valley. They are characterized by an abundance of limestone
material of diverse structure, silt, and coarse sand, as well as gravel
and pebbles mixed with clay in places.
C) A large dejection cone containing alluvial deposits,
formed for the most part 5,000 years ago, is composed of aalenian
shale (Middle Jurassic or Dogger) and metalimestone carried down from
Haut-de-Cry and Ardèvaz by the Losentse, Cry and Saint-André
torrents. The cone contains no trace of Rhodanian moraine. It has a relatively
gentle downward slope and is quite permeable to water.
Market gardens and fruit orchards are located along the banks of the
Rhône River in the lower section of the immense Losentse dejection
cone.
At the foot of the vineyards lies the village of St-Pierre-de-Clages,
known as Switzerland’s “village of books” and home to
a famous Roman church built by Benedictine monks in the 9th century along
the route taken by pilgrim’s to St-Jacques de Compostelle.
Above the village are the vineyards, the jewel of the region’s
largest winegrowing commune. These 430 hectares represent almost 10% of
vineyards in Valais (5,000 hectares), which itself is home to a third
of all winegrowing in Switzerland. The gentle slopes of the dejection
cone host 90% of Chamoson vineyards, with the rest planted in a series
of terraces on steeper hillsides. At the top of the cone, where the plain
meets the mountain, is the hamlet of Le Grugnay, home to Switzerland’s
museum of speleology.
The forest takes over as the slopes rise above this point. Anyone seeking
peace and quiet can head for the hamlets of Némiaz and Vérines,
havens of calm nestled in the mountain foothills at the base of the steep
cliffs of Haut-de-Cry. Higher yet is Les Mayens de Chamoson, with its
quaint chalets dotting the mountainside and small hotels forming part
of a modest tourist industry based on the hot springs and ski slopes of
Ovronnaz. Visitors can also continue on to Rambert hut, the starting point
for a hiking tour of the Muverans.
Set in the heart of the Swiss Alps along the right bank of the Rhône
River in Valais, the village of Chamoson (home of the Foundation) lies
12 km from Sion, capital of the canton, and 17 km from the cultural centre
of Martigny.
How to get there:
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By car:
From highway A 9, take the Riddes/Chamoson/Leytron exit and
follow the indications to Leytron-Chamoson. At the exit for
Leytron, follow the Route du Vin. |
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By train:
Take the regional train from Sion or Martigny and get off at
the Chamoson station. |
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By bus:
Take the Chamoson bus line from the Sion or Martigny
station. There are stops at St-Pierre-de-Clages, Grugnay,
Les Mayens and Ovronnaz. |
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Map taken from the Chamoson tourism
guide “Venir à Chamoson” |
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MAP.SEARCH.CH |
In addition to its administrative centre, Chamoson includes the
villages of Grugnay, Némiaz, St-Pierre-de-Clages, Vérines,
and les Mayens de Chamoson, which have a total population
of 2,900. Together with the communes of Ardon, Vétroz and
Nendaz, Chamoson is part of the District of Conthey.
Chamoson’s 3,500 hectares comprise orchards, vineyards, huts,
mountain pastures, and rock formations. The splendid landscape is
surprisingly diverse as it rises from the banks of the Rhône
(480 m) to the towering summits of the steep Haut-de-Cry and the
majestic Grand Muveran, which reaches 3,051 metres.
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