Puy De Sancy
Puy de Sancy (, ; , ) is the highest mountain in the Massif Central, in Puy-de-Dôme departement of south central France. 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 cable cars and ski lifts 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. On Christmas Day in late 1965, a cable car accident on a newer line 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 and on to the Gironde estuary The Gironde estuary ( , U ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Monts Dore
The Monts Dore () are the remnant peaks of a volcanic massif situated near the center of the Massif Central, in the Auvergne region of France. They form a picturesque mountainous region, dotted with lakes, thermal springs and romanesque churches. The massif is an integral part of the Parc des Volcans d'Auvergne, and is known for its alpine ski areas and hiking trails. Geology The massif is much older than the nearby chaîne des Puys, dating to the end of the Tertiary era. It is a deeply eroded stratovolcano, similar to the Cantal massif to the south, but more reduced in area and volume. Its history began about 3 million years ago with a Plinian eruption that created a large caldera, the contours of which are no longer clearly defined. This eruption resulted in the emission of ignimbrite rhyolitic pumice that covered over of land. Afterwards, phonolite domes were created on the exterior of the caldera. A period of calm lasting between 1 and 1.5 million years ensued, succeeded ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Christmas
Christmas is an annual festival commemorating Nativity of Jesus, the birth of Jesus Christ, observed primarily on December 25 as a Religion, religious and Culture, cultural celebration among billions of people Observance of Christmas by country, around the world. A liturgical year, liturgical feast central to Christianity, Christmas preparation begins on the Advent Sunday, First Sunday of Advent and it is followed by Christmastide, which historically in the West lasts Twelve Days of Christmas, twelve days and culminates on Twelfth Night (holiday), Twelfth Night. Christmas Day is a public holiday in List of holidays by country, many countries, is observed religiously by a majority of Christians, as well as celebrated culturally by many non-Christians, and forms an integral part of the annual Christmas and holiday season, holiday season. The traditional Christmas narrative recounted in the New Testament, known as the Nativity of Jesus, says that Jesus was born in Bethlehem, in ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Pleistocene Volcanoes
The Pleistocene ( ; referred to colloquially as the ''Ice Age'') is the geological epoch that lasted from 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 () 'most' and (; Latinized as ) 'new'. The aridification and cooling trends of the preceding Neogene were continued in the Pleistocene. The climate was strongly variable depending on the glacial cycle, oscillating between cold glacial periods and warmer interglacials, with the sea levels being up to lower th ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Mountains Of Puy-de-Dôme
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 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 climate, mountains te ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Landforms Of Auvergne-Rhône-Alpes
A landform is a land feature on the solid surface of the Earth or other planetary body. They may be natural or may be anthropogenic (caused or influenced by human activity). 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 oceanic basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, structure stratification, rock exposure, and soil type. Gross physical features or landforms include intuitive elements such as berms, cliffs, hills, mounds, peninsulas, ridges, rivers, valleys, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodi ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Inactive Volcanoes
Inactive is a TRPV channel in invertebrates Invertebrates are animals that neither develop nor retain a vertebral column (commonly known as a ''spine'' or ''backbone''), which evolved from the notochord. It is a paraphyletic grouping including all animals excluding the chordate subphylum .... Inactive mutant flies show locomotor and hearing deficits. References Ion channels Nervous system {{animal-anatomy-stub ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Landforms Of Puy-de-Dôme
A landform is a land feature on the solid surface of the Earth or other planetary body. They may be natural or may be anthropogenic (caused or influenced by human activity). 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 oceanic basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, structure stratum, stratification, rock exposure, and soil type. Gross physical features or landforms include intuitive elements such as berms, cliffs, hills, mounds, peninsulas, ridges, rivers, valleys, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic b ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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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 ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Gironde Estuary
The Gironde estuary ( , US usually ; , ; , ) 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. Giving its name to 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 in size with a lighthouse to aid navigation in the estuary. Vines and maize are grown there. The Île Sans-Pain and Île Bouchaud are now ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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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, Somerset, 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, and comes from the Belgian town Spa, Belgium, Spa. Spa towns by country 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 Daylesfo ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Dordogne (river)
The Dordogne (; ) is a river in south-central and southwest France. It is long. The Dordogne and its watershed were designated Man and the Biosphere Programme, Biosphere Reserve by UNESCO on 11 July 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 (France), Le Mont-Dore: the ''Dore'' and the ''Dogne''. It flows generally west nearly through the Limousin (région), Limousin and Périgord regions before flowing into the Gironde estuary, 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 severa ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |