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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] |
Miocene Stratovolcanoes
The Miocene ( ) is the first geological epoch of the Neogene Period and extends from about (Ma). The Miocene was named by Scottish geologist Charles Lyell; the name comes from the Greek words (', "less") and (', "new") and means "less recent" because it has 18% fewer modern marine invertebrates than the Pliocene has. The Miocene is preceded by the Oligocene and is followed by the Pliocene. As Earth went from the Oligocene through the Miocene and into the Pliocene, the climate slowly cooled towards a series of ice ages. The Miocene boundaries are not marked by a single distinct global event but consist rather of regionally defined boundaries between the warmer Oligocene and the cooler Pliocene Epoch. During the Early Miocene, the Arabian Peninsula collided with Eurasia, severing the connection between the Mediterranean and Indian Ocean, and allowing a faunal interchange to occur between Eurasia and Africa, including the dispersal of proboscideans into Eurasia. During the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stratovolcanoes Of Metropolitan France
A stratovolcano, also known as a composite volcano, is a Volcanic cone, conical volcano built up by many layers (strata) of hardened lava and tephra. Unlike shield volcanoes, stratovolcanoes are characterized by a steep profile with a summit crater and periodic intervals of explosive eruptions and effusive eruptions, although some have collapsed summit craters called calderas. The lava flowing from stratovolcanoes typically cools and hardens before spreading far, due to high viscosity. The magma forming this lava is often felsic, having high-to-intermediate levels of silica (as in rhyolite, dacite, or andesite), with lesser amounts of less-viscous Igneous rock#Mineralogical classification, mafic magma. Extensive felsic lava flows are uncommon, but have travelled as far as . Stratovolcanoes are sometimes called composite volcanoes because of their composite stratified structure, built up from sequential outpourings of erupted materials. They are among the most common types of v ... [...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] |
Salers Cheese
Salers (french: Le Salers) is a French semi-hard cheese originating from Salers, in the volcanic region of the Cantal mountains of the Massif Central, Auvergne, central France. It is a pressed, uncooked cheese, sometimes made from Salers cow's milk (it's then called "Tradition Salers"), between 15 April and 15 November. It is circular in shape, formed in rounds weighing around . The cheese is aged in caves at temperatures ranging from 6–12 °C (43–54 °F) for a minimum of 3 months, and up to 45 months. Salers de Buron Traditional is only made in stone huts (called ''burons'' in the Auvergne) in the summer months with milk exclusively from the Salers cow. It must also be made in the traditional wooden ''gerle''. It is best eaten between September and March, after an ageing time of nine months, but it is also excellent all year round. History Salers has been produced since ancient times. It is estimated to have been produced in this region for at least 2,000 years. Salers came ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cantal Cheese
Cantal cheese is an uncooked firm cheese produced in the Auvergne region of central France: more particularly in the ''département'' of Cantal (named after the Cantal mountains) as well as in certain adjoining districts. Cantal cheese was granted Appellation d'Origine Contrôlée certification in 1956. One of the oldest cheeses in France, Cantal dates back to the times of the Gauls. It came to prominence when Marshal Henri de La Ferté-Senneterre served it at the table of Louis XIV of France. Senneterre is also responsible for the introduction of Saint-Nectaire and Salers. Composition There are two types of Cantal cheese: ''Cantal Fermier'', a farmhouse cheese made from raw milk; and ''Cantal Laitier,'' a commercial, mass-produced version made from pasteurized milk. Both have to adhere to the same strict quality controls. The cheese is made only using milk from hay-fed Salers cows, and is only harvested from November 15 to April 15. The summer milk of the same cows grazing on m ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Salers (cattle)
250px, Salers cattle The Salers (french: race de Salers or ''La Salers''; plural: ''Les Salers'') is a breed of cattle which originated in Cantal in the Massif Central of France. They are a large breed, with the female weighing between 700 and 750 kg (1,543 to 1,653 lb) and standing 1.40 m (4.6 feet) tall. They have a thick, mahogany red or black coat, and long, lyre-shaped, light-coloured horns. A small percentage is naturally born without horns (polled). In the 19th century, the breeder Ernest Tyssandier d'Escous set about to better the breed by selective breeding. Originally bred for work, this dual-purpose breed was especially appreciated for its ability to withstand extreme variations in temperature, its fertility, its ease of breeding, its milk (even if the presence of the calf was required to milk it), and its meat. In Cantal, the farmers practise mountain pasture, with the herd passing summer at altitude in the mountains. A female can produce almost 3,000& ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alagnon
The Alagnon (''Alanhon'' in Occitan), also spelled ''Allagnon'', is an river in south-central France. It is a left tributary of the river Allier. Its source is near the village of Laveissière, near the Plomb du Cantal in the Massif Central. The Alagnon flows generally northeast through the following departments and towns: * Cantal: Murat, Massiac * Haute-Loire: Lempdes-sur-Allagnon * Puy-de-Dôme: Beaulieu The Alagnon flows into the river Allier at Auzat-la-Combelle Auzat-la-Combelle () is a commune in the Puy-de-Dôme department in Auvergne-Rhône-Alpes in central France. It is in the canton of Brassac-les-Mines. Population See also * Communes of the Puy-de-Dôme department The following is a list .... References Rivers of France Rivers of Auvergne-Rhône-Alpes Rivers of Cantal Rivers of Haute-Loire Rivers of Puy-de-Dôme {{France-river-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cirque
A (; from the Latin word ') is an amphitheatre-like valley formed by glacial erosion. Alternative names for this landform are corrie (from Scottish Gaelic , meaning a pot or cauldron) and (; ). A cirque may also be a similarly shaped landform arising from fluvial erosion. The concave shape of a glacial cirque is open on the downhill side, while the cupped section is generally steep. Cliff-like slopes, down which ice and glaciated debris combine and converge, form the three or more higher sides. The floor of the cirque ends up bowl-shaped, as it is the complex convergence zone of combining ice flows from multiple directions and their accompanying rock burdens. Hence, it experiences somewhat greater erosion forces and is most often overdeepened below the level of the cirque's low-side outlet (stage) and its down-slope (backstage) valley. If the cirque is subject to seasonal melting, the floor of the cirque most often forms a tarn (small lake) behind a dam, which marks the down ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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