Puy De Sancy
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Puy De Sancy
Puy de Sancy (, ; oc, label=Auvergnat, Puèi de la Crotz , ) is the highest mountain in the Massif Central. It is part of an ancient stratovolcano which has been inactive for about 220,000 years. The northern and southern slopes are used for skiing, and a number of cablecars and skilifts ascend the mountain. Skiing has been practised on the mountain since the early 20th century. Two local priests traversed the Puy de Sancy on skis in 1905. In 1936, a cable car link was built from Mont-Dore to one of the needles just below the summit. In December 1965, a cable car accident injured ten passengers and killed seven others. Super-Besse is another ski resort, located on the southwestern slope. The valley to the north is also the source of two streams called ''Dore'' and ''Dogne'', which unite to form the Dordogne, which flows through the nearby spa town of Mont-Dore Mont-Dore
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Massif Central
The (; oc, Massís Central, ; literally ''"Central Massif"'') is a highland region in south-central France, consisting of mountains and plateaus. It covers about 15% of mainland France. Subject to volcanism that has subsided in the last 10,000 years, these central mountains are separated from the Alps by a deep north–south cleft created by the Rhône river and known in French as the ' (literally "Rhône furrow"). The region was a barrier to transport within France until the opening of the A75 motorway, which not only made north–south travel easier, but also opened access to the massif itself. Geography and geology The is an old massif, formed during the Variscan orogeny, consisting mostly of granitic and metamorphic rocks. It was powerfully raised and made to look geologically younger in the eastern section by the uplift of the Alps during the Paleogene period and in the southern section by the uplift of the Pyrenees. The massif thus presents a strongly asymmet ...
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Super-Besse
Super Besse is a winter sports resort located in Massif Central, France. Geography Super Besse located in the commune of Besse-et-Saint-Anastaise (''Parc naturel régional des volcans d'Auvergne'' in the department of Puy-de-Dôme, Auvergne). Situated approximately 50 km from Clermont-Ferrand, it is located at an altitude of 1350 m on the slopes of Puy de Sancy, Puy de la Perdrix and Puy Ferrand. Facilities The on piste skiing consists of 43 km distributed on 27 tracks (5 green, 9 blue, 9 red and 4 black) between 1300 m and 1840 m altitude, on the south-eastern slope of Puy de Sancy. It contains 21 ski lifts. It also includes 125 km of cross-country skiing. The resort includes: * 1 funitel with 20 places (new in 2008) * 4 chair-lifts * 16 ski-lifts. Tour de France Super-Besse hosted the first mountain finish of the 2008 Tour de France. The finish was at an altitude of 1289 m, whereas in previous years the finish was at 1350 m. Tour de France stage finish ...
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Pleistocene Volcanoes
The Pleistocene ( , often referred to as the ''Ice age'') is the geological epoch that lasted from about 2,580,000 to 11,700 years ago, spanning the Earth's most recent period of repeated glaciations. Before a change was finally confirmed in 2009 by the International Union of Geological Sciences, the cutoff of the Pleistocene and the preceding Pliocene was regarded as being 1.806 million years Before Present (BP). Publications from earlier years may use either definition of the period. The end of the Pleistocene corresponds with the end of the last glacial period and also with the end of the Paleolithic age used in archaeology. The name is a combination of Ancient Greek grc, label=none, πλεῖστος, pleīstos, most and grc, label=none, καινός, kainós (latinized as ), 'new'. At the end of the preceding Pliocene, the previously isolated North and South American continents were joined by the Isthmus of Panama, causing a faunal interchange between the two reg ...
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Mountains 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 and ...
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Landforms Of Auvergne-Rhône-Alpes
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateaux, and plains are the fo ...
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Inactive Volcanoes
Inactive is a TRPV channel in invertebrates Invertebrates are a paraphyletic group of animals that neither possess nor develop a vertebral column (commonly known as a ''backbone'' or ''spine''), derived from the notochord. This is a grouping including all animals apart from the chordate .... Inactive mutant flies show locomotor and hearing deficits. References Ion channels Nervous system {{animal-anatomy-stub ...
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Landforms Of Puy-de-Dôme
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateaux, and plains are the fou ...
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Puy Sancy Sud
Puy () is a geological term used locally in the Auvergne, France for a volcanic hill. The word derives from the Provençal ''puech'', meaning an isolated hill, coming from Latin ''podium'', which has given also ''puig'' in Catalan, ''poggio'' in Italian, ''poio'' in Galician and Portuguese. Most of the puys of central France are small cinder cones, with or without associated lava, whilst others are domes of trachytic rock, like the of the Puy-de-Dôme. The puys may be scattered as isolated hills, or, as is more usual, clustered together, sometimes in lines. The chain of puys in central France probably became extinct in late prehistoric time. Other volcanic hills more or less like those of Auvergne are also known to geologists as puys; examples may be found in the Eifel and in the small cones on the Bay of Naples, whilst the relics of puys denuded by erosion are numerous in the Swabian Alps of Württemberg, as pointed out by W. Branco. Sir A. Geikie has shown that the puy typ ...
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Gironde Estuary
The Gironde estuary ( , US usually ; french: estuaire de la Gironde, ; oc, estuari de aGironda, ) is a navigable estuary (though often referred to as a river) in southwest France and is formed from the meeting of the rivers Dordogne and Garonne just downstream of the centre of Bordeaux. Covering around , it is the largest estuary in western Europe. Named after the French ''département'' Gironde, the Gironde estuary is approximately long and 3–12 km (2–7 miles) wide. It is subject to very strong tidal currents and great care is needed when navigating the estuary by any size or type of boat. Since 2015, the Gironde estuary has been part of the Gironde estuary and Pertuis sea Marine Nature Park. Islands of the Gironde Within the estuary between the Pointe de Grave at the seaward end and the Bec d'Ambès are a series of small islands. The Île de Patiras is 200  ha in size with a lighthouse to aid navigation in the estuary. Vines and maize are gro ...
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Spa Town
A spa town is a resort town based on a mineral spa (a developed mineral spring). Patrons visit spas to "take the waters" for their purported health benefits. Thomas Guidott set up a medical practice in the English town of Bath in 1668. He became interested in the curative properties of the hot mineral waters there and in 1676 wrote ''A discourse of Bathe, and the hot waters there. Also, Some Enquiries into the Nature of the water''. This brought the purported health-giving properties of the waters to the attention of the aristocracy, who started to partake in them soon after. The term ''spa'' is used for towns or resorts offering hydrotherapy, which can include cold water or mineral water treatments and geothermal baths. Argentina *Termas de Rio Hondo *Presidencia Roque Sáenz Peña Australia There are mineral springs in the Central Highlands of Victoria. Most are in and around Daylesford and Hepburn Springs. Daylesford and Hepburn Springs call themselves 'Spa Countr ...
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Dordogne (river)
The Dordogne (; oc, Dordonha) is a river in south-central and southwest France. It is long. The Dordogne and its watershed were designated Biosphere Reserve by UNESCO on July 11 2012. Geography The river rises on the flanks of the Puy de Sancy at above sea level in the mountains of Auvergne, from the confluence of two small torrents above the town of Le Mont-Dore: the ''Dore'' and the ''Dogne''. It flows generally west about through the Limousin and Périgord regions before flowing into the Gironde, its common estuary with the Garonne, at the Bec d'Ambès ("Ambès beak"), north of the city of Bordeaux. Nature The Dordogne is one of the few rivers in the world that exhibit the phenomenon of a tidal bore, known as a mascaret. The upper valley of the Dordogne is a series of deep gorges. The cliffs, steep banks, fast flowing water and high bridges attract both walkers and drivers. In several places the river is dammed to form long, deep lakes. Camp sites and holiday homes ...
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Mont-Dore
Mont-DoreCommune de Mont-Dore (63236)
code officiel géographique, INSEE
(; ''Mont Dòr'' in , and ''Mont-Dore-les-Bains''), in common usage ''Le Mont-Dore'', is a in the department in Auvergne-Rhône-Alpes
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