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Col Du Grapillon
The Col du Grapillon (or col de Grapillon) is a mountain pass located above sea level in the Chartreuse Mountains between La Cochette () to the south, and Mont Outheran () to the north Access The pass is available only to hikers. It connects Le Désert d'Entremont (Entremont-le-Vieux district) to Saint-Thibaud-de-Couz, and it's the southern access path of the Mont Outheran and northern access path of La Cochette. The easiest access is from the hamlet of les Bruyères on the D45, north of Col de la Cluse. Environmental protection The Col du Grapillon is part of the natural area of ecological, faunistic and floristic interest of Mont Outheran Mont Outheran (1,676 m) is a mountain of the Chartreuse Mountains in the French Prealps, Savoie, France. Geography The Mont Outheran is a narrow plateau, lying several kilometers in the north-south direction between the Col du Grapillon at the so .... References Mountain passes of Auvergne-Rhône-Alpes Mountain passes of the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Savoie
Savoie (; Arpitan: ''Savouè'' or ''Savouè-d'Avâl''; English: ''Savoy'' ) is a department in the Auvergne-Rhône-Alpes region, Southeastern France. Located in the French Alps, its prefecture is Chambéry. In 2019, Savoie had a population of 436,434.Populations légales 2019: 73 Savoie INSEE Together with , it is one of the two departments of the historical region of Savoy; the Duchy of Savoy was annexed by France in 1860, following the signature of the [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chartreuse Mountains
The Chartreuse Mountains (french: massif de la Chartreuse ) are a mountain range in southeastern France, stretching from the city of Grenoble in the south to the Lac du Bourget in the north. They are part of the French Prealps, which continue as the Bauges to the north and the Vercors to the south. Etymology The name ''Chartreuse'' is derived from the village now known as Saint-Pierre-de-Chartreuse, earlier ''Catorissium'', ''Cantourisa'', ''Caturissium'', and ''Chatrousse''. It appears to be of Gaulish origin; and is perhaps related to the name of the Caturiges tribe. Geography The mountain range rises between Grenoble (south), Chambéry (north), Voiron and Saint-Laurent-du-Pont (west) and Grésivaudan (''Isère valley'', east) Main summits Summits of the Chartreuse Mountains include: *Chamechaude, *Dent de Crolles, * Les Lances de Malissard * Grand Som, * Dôme de Bellefont * Piton de Bellefont *Mont Granier, * La Grande Sure, * Le Charmant Som * Sommet du Pinet ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Pass
A mountain pass is a navigable route through a mountain range or over a ridge. Since many of the world's mountain ranges have presented formidable barriers to travel, passes have played a key role in trade, war, and both Human migration, human and animal migration throughout history. At lower elevations it may be called a hill pass. A mountain pass is typically formed between two volcanic peaks or created by erosion from water or wind. Overview Mountain passes make use of a gap (landform), gap, saddle (landform), saddle, col or notch (landform), notch. A topographic saddle is analogous to the mathematical concept of a saddle surface, with a saddle point marking the highest point between two valleys and the lowest point along a ridge. On a topographic map, passes are characterized by contour lines with an hourglass shape, which indicates a low spot between two higher points. In the high mountains, a difference of between the summit and the mountain is defined as a mountain pas ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
La Cochette
La Cochette (or Pointe de la Cochette) is a mountain of the Chartreuse Mountains culminating at 1618 m above sea level and located at the edge of Corbel, of Saint-Jean-de-Couz and of Entremont-le-Vieux in Savoie. Geography La Cochette is part of the Mount Outheran Range. The link extends to the south by its south antecime, the tip of the Grand Crêt, and ends at the Pointe de Thivelet. The rocky crest of La Cochette is formed by limestone Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms whe ...s of Fontanil Access Access to the tip of the Cochette passes through the col du Grapillon. Environmental protection La Cochette is part of the Regional Natural Park of Chartreuse and the natural area of ecological, faunistic and floristic interest type II of the Chartreuse massif. R ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mont Outheran
Mont Outheran (1,676 m) is a mountain of the Chartreuse Mountains in the French Prealps, Savoie, France. Geography The Mont Outheran is a narrow plateau, lying several kilometers in the north-south direction between the Col du Grapillon at the south and the Col du Planet at the north. It is surrounded by cliffs on all sides. The west cliff defines the territory of the commune of Saint-Thibaud-de-Couz. Much of Mont Outheran is wholly owned by the township. The Mont Outheran consists of urgonian limestone Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms whe .... Mountains of Savoie Mountains of the Alps Chartreuse Mountains {{Savoie-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Le Désert D'Entremont
Le Desert d'Entremont is a winter sports resort in the commune of Entremont-le-Vieux located in the Chartreuse Mountains. It lies between the communes of Entremont-le-Vieux and Corbel. Introduction In winter, with presence of snow, we can practice downhill skiing , cross country skiing , sled , snowshoes Snowshoes are specialized outdoor gear for walking over snow. Their large footprint spreads the user's weight out and allows them to travel largely on top of rather than through snow. Adjustable bindings attach them to appropriate winter footwe ..., etc. History The ski station was built in 1968. Events Cross country skiing nights are sometimes organized. The tracks are lighted during the events. References Ski stations in France Tourist attractions in Savoie Sports venues in Savoie {{Savoie-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Entremont-le-Vieux
Entremont-le-Vieux ( Arpitan: ''Entremont-le-Viûx'') is a commune in the Savoie department in the Auvergne-Rhône-Alpes region in Southeastern France. In 2019, it had a population of 644. Geography Entremont-le-Vieux is a landlocked village close to many water streams and winter sports resorts (including Le Désert d'Entremont). It is mainly the ''Cozon'' river and its tributaries that flow into the valley that have shaped the landscape. One of the main features of the town is the dispersion of a set of houses in 26 villages. The main passes located in the town are the col de la Cluse, the col du Cucheron southwest and the col du Mollard northwest. Neighboring municipalities Neighboring communes of Entremont-le-Vieux are Saint-Pierre d'Entremont in Savoie, Sainte-Marie-du-Mont, Saint-Jean-de-Couz and Corbel. History The parish of Notre-Dame d'Epernay is the lordship of the ''Entremonts valley''. The church of Entremont-le-Vieux, Notre-Dame d'Epernay, was rebuilt in the mi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saint-Thibaud-de-Couz
Saint-Thibaud-de-Couz () is a commune of the Savoie department in the Auvergne-Rhône-Alpes region in south-eastern France. Geography The village of Saint-Thibaud-de-Couz is located in the middle valley of the Hyères between Mont Grêle (1425 m) and Mont Outheran (1,676 m). Forests cover half of the township. The township is part of the Communauté de communes Cœur de Chartreuse. Toponymy In the eleventh century, a Breton monk named Theobaldus built for pilgrims and travelers a "Hostellerie priory", at a place called ''Pre Chartreux'' between the ''Gencourt'' and the ''Poulemonts''. Theobaldus gave the town its name (Thibaud), we called then the town under the name of Saint Thibaud. Full name ''Saint-Thibaud-de-Couz'' is mentioned for the first time in Latin in 1497 in the cartulary Labaudie "Parrochia Sancti theobaldi de Couz". The name Couz, which means "pass" was used to refer to the ''Hyères valley'' until the ''Caves parade''. History After the planning of the caves par ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Col De La Cluse
The Col de la Cluse is a mountain pass located 1,169 m above sea level in the Chartreuse Mountains. It connects Le Désert d'Entremont (commune of Entremont-le-Vieux) to Corbel, Savoie, France. The main road of the pass is the D45. In winter, It is a departure to the cross country ski slopes. In summer, it is the start of a two-hour hike to access to Roche Veyrand (1,429 m), overlooking Saint-Pierre d'Entremont in Savoie. The nearby Roc de Gleisin can also be reached. It is one of the access roads to the Col du Grapillon The Col du Grapillon (or col de Grapillon) is a mountain pass located above sea level in the Chartreuse Mountains between La Cochette () to the south, and Mont Outheran () to the north Access The pass is available only to hikers. It connects ..., to the east. References Mountain passes of Auvergne-Rhône-Alpes Mountain passes of the Alps {{Savoie-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Passes Of Auvergne-Rhône-Alpes
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
