|
Puy Griou
The Puy Griou is a summit at an altitude of 1,690 meters in the Mounts of Cantal, located on the ridge line between the valleys of the Cère and the , partially situated in the municipalities of Saint-Jacques-des-Blats and Mandailles. Toponymy The summit is called "Puei Griu" in Aurillac Occitan. In this dialect, ''griu'' comes from ''griea'', which means "difficult to climb." In the Occitan auvergnat spoken further north of the mountain, it is called ''Puei de Grion''. Geology Due to its position in the center of the Monts du Cantal and its very slender conical shape, Puy Griou was long considered to be the eroded chimney of the Cantal volcano. However, it has since lost this status, and geologists now consider it to be a phonolite dome occupying a central position similar to other peaks in the massif such as . It is believed to have formed approximately 6 million years ago, following the paroxysmal eruptive phases experienced by the Cantal between 8.5 Ma and 6.5 Ma. Duri ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mounts Of Cantal
The Mounts of Cantal (or Volcanoes of Cantal; french: Monts du Cantal ) are a mountainous massif in the mid-west of the Massif Central, France, made up of the remnants of the largest stratovolcano of Europe, which was formed from 13 million years ago and last erupted approximately 2 million years ago. However, the main part of the volcanic activity was concentrated between 8.5 and 7 million years ago. Thereafter, the original volcano was largely eroded, massive landslides occurred, and it was further eroded by glaciers and water. Geomorphology The stratovolcano of Cantal is the widest in Europe. It is roughly circular with a diameter between . Its highest point is the Plomb du Cantal (), located in the eastern part of the massif. Around 20 valleys have been formed in the range, radiating out from the centre and cutting the basaltic plateau into triangular pieces called '' planèzes''. These valleys were occupied by glaciers during the last ice age, which explains their U-shape. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Occitan Language
Occitan (; oc, occitan, link=no ), also known as ''lenga d'òc'' (; french: langue d'oc) by its native speakers, and sometimes also referred to as ''Provençal'', is a Romance languages, Romance language spoken in Southern France, Monaco, Italy's Occitan Valleys, as well as Spain's Val d'Aran; collectively, these regions are sometimes referred to as Occitania, Occitània. It is also spoken in Calabria (Southern Italy) in a linguistic enclave of Cosenza area (mostly Guardia Piemontese). Some include Catalan language, Catalan in Occitan, as the Linguistic distance, distance between this language and some Occitan dialects (such as the Gascon language) is similar to the distance between different Occitan dialects. Catalan was considered a dialect of Occitan until the end of the 19th century and still today remains its closest relative. Occitan is an official language of Catalonia, where a subdialect of Gascon known as Aranese dialect, Aranese is spoken in the Val d'Aran. Since Sept ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of The Massif Central
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Le Lioran
Le Lioran is a small mountain resort in the heart of continental France. It consists of the original settlement of Le Lioran in the valley bottom as well as the settlements of Prairie de Sagnes, Font d'Alagon, Font de Cère, and Prat du Bouc, all of which are geared towards the mountain tourism market. The largest of these is the Prairie de Sagnes, now known as Super-Lioran; most facilities and accommodation are concentrated there. One of the few remaining resorts in central France, it has grown to become one of the biggest and most advanced resorts in the Massif Central. There is a wide range of sporting and leisure activities on offer in addition to the more traditional winter sports and the wealth of lodging and other services available. There is a heavy emphasis on the all year round nature of the resort, although, inevitably, the resort is busiest in the winter season. Geography Within France it is administratively located in the ''commune'' of Laveissière, the '' canton'' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
GR 400
The GR 400 is a long-distance walking route within the Grande Randonnée network in France. It is not a linear route, but a series of five circuits, all within the Monts de Cantal area of the Massif Central. The circuits interconnect with, and sometimes follow the same route as, the GR 4, one of the spine paths of the network, and also with a subsidiary section of the Via Podiensis St James's Way route. The walking is described as "within the range of any good hiker accustomed to walking in mountain country and to carrying a rucksack""Volcan du Cantal", TopoGuide of the Fedération Française de la Randonée Pédestrien, The five circuits are: * Alagnon valley loop, starting and finishing at Murat (44 km) * Cère valley loop, starting and finishing at Super-Lioran (39 km) * Jordanne valley loop, starting and finishing at Mandailles-Saint-Julien (35 km) *Le Falgoux loop, starting and finishing at Le Falgooux (39 km) *Le Claux valley loop, starting and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Quaternary
The Quaternary ( ) is the current and most recent of the three periods of the Cenozoic Era in the geologic time scale of the International Commission on Stratigraphy (ICS). It follows the Neogene Period and spans from 2.58 million years ago to the present. The Quaternary Period is divided into two epochs: the Pleistocene (2.58 million years ago to 11.7 thousand years ago) and the Holocene (11.7 thousand years ago to today, although a third epoch, the Anthropocene, has been proposed but is not yet officially recognised by the ICS). The Quaternary Period is typically defined by the cyclic growth and decay of continental ice sheets related to the Milankovitch cycles and the associated climate and environmental changes that they caused. Research history In 1759 Giovanni Arduino proposed that the geological strata of northern Italy could be divided into four successive formations or "orders" ( it, quattro ordini). The term "quaternary" was introduced by Jules Desnoye ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Phonolite
Phonolite is an uncommon extrusive rock, of intermediate chemical composition between felsic and mafic, with texture ranging from aphanitic (fine-grained) to porphyritic (mixed fine- and coarse-grained). Phonolite is a variation of the igneous rock trachyte that contains nepheline or leucite rather than quartz. Its intrusive equivalent is nepheline syenite. Phonolite is typically fine grained and compact. The name ''phonolite'' comes from the Ancient Greek meaning "sounding stone" due to the metallic sound it produces if an unfractured plate is hit; hence, the English name ''clinkstone'' is given as a synonym. Formation Unusually, phonolite forms from magma with a relatively low silica content, generated by low degrees of partial melting (less than 10%) of highly aluminous rocks of the lower crust such as tonalite, monzonite and metamorphic rocks. Melting of such rocks to a very low degree promotes the liberation of aluminium, potassium, sodium and calcium by melting of f ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Auvergnat
or (endonym: ) is a northern dialect of Occitan spoken in central and southern France, in particular in the former administrative region of Auvergne. Currently, research shows that there is not really a true Auvergnat dialect but rather a vast northern Occitan linguistic area. The word "Auvergnat" is above all a local historiographical creation. According to linguist Jean Roux, "It is by simplification that we use this term, because in no case Auvergnat can be considered as an autonomous linguistic entity". With around 80,000 speakers in the Auvergne region at the beginning of the 21st century, it is considered to be severely endangered. Classification Auvergnat falls under the following categories and subcategories: Indo-European, Italic, Romance, Italo-Western, Gallo-Iberian, Gallo-Romance, Occitan. History Several troubadours were from the Auvergne, including Castelloza, Dalfi d'Alvernhe, the Monje de Montaudon, the Vesques de Clarmon, Peire d'Alvernhe, Peire Rogier ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Aurillac
Aurillac (; oc, Orlhac ) is the prefecture of the Cantal department, in the Auvergne-Rhône-Alpes region of France. The inhabitants of the commune are known as ''Aurillacois'' or ''Aurillacoises''. Geography Aurillac is at above sea level and located at the foot of the Cantal mountains in a small Sedimentary basin. The city is built on the banks of the Jordanne, a tributary of the Cère. It is south of Paris and north of Toulouse. Aurillac was part of a former Auvergne province called Haute-Auvergne and is only away from the heart of the Auvergne Volcano Park. Access to the commune is by numerous roads including the D922 from Naucelles in the north, the D17 from Saint-Simon in the north-east, Route nationale N122 from Polminhac in the east which continues to Sansac-de-Marmiesse in the south-west, the D920 to Arpajon-sur-Cère in the south-east, and the D18 to Ytrac in the west. Aurillac station, in the centre of town, lies on the Figeac-Arvant railway. It has rail con ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mandailles-Saint-Julien
Mandailles-Saint-Julien (; oc, Mandalha e Sant Julian) is a commune in the Cantal department Department may refer to: * Departmentalization, division of a larger organization into parts with specific responsibility Government and military *Department (administrative division), a geographical and administrative division within a country, ... in south-central France. Population See also * Communes of the Cantal department References Communes of Cantal Cantal communes articles needing translation from French Wikipedia {{Cantal-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saint-Jacques-des-Blats
Saint-Jacques-des-Blats (; Auvergnat: ''Sant Jaume dels Blats'') is a commune in the Cantal department in south-central France. Population See also *Communes of the Cantal department The following is a list of the 246 communes of the Cantal department of France. Intercommunalities The communes cooperate in the following intercommunalities (as of 2020):Communes of Cantal Cantal communes articles needing translation from French Wikipedia {{Cantal-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
