To install click the Add extension button. That's it.

The source code for the WIKI 2 extension is being checked by specialists of the Mozilla Foundation, Google, and Apple. You could also do it yourself at any point in time.

4,5
Kelly Slayton
Congratulations on this excellent venture… what a great idea!
Alexander Grigorievskiy
I use WIKI 2 every day and almost forgot how the original Wikipedia looks like.
What we do. Every page goes through several hundred of perfecting techniques; in live mode. Quite the same Wikipedia. Just better.
.
Leo
Newton
Brights
Milds

Massif Central

From Wikipedia, the free encyclopedia

Massif Central
View of Puy de Sancy, the highest peak in the Massif Central
Highest point
PeakPuy de Sancy
Elevation1,886 m (6,188 ft)
Coordinates45°31′42″N 2°48′51″E / 45.52833°N 2.81417°E / 45.52833; 2.81417
Naming
Native nameMassís Central (Occitan)
PronunciationUK: /ˌmæsfsɒ̃ˈtrɑːl/, US: /mæˌsf-,-sɛnˈ-,məˌsfsɑːnˈ-/[1][2][3]
French: [masifsɑ̃tʁal]
Occitan: [maˈsissenˈtɾal]
Geography
CountryFrance
RegionsAuvergne-Rhône-Alpes, Bourgogne-Franche-Comté, Nouvelle-Aquitaine and Occitania
Range coordinates46°N 3°E / 46°N 3°E / 46; 3

The Massif Central (French pronunciation: [masifsɑ̃tʁal])[4] 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 sillon rhodanien (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 Massif Central 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 asymmetrical elevation profile with highlands in the south and in the east (Cévennes) dominating the valley of the Rhône and the plains of Languedoc and, by contrast, the less elevated region of Limousin in the northwest.

These tectonic movements created faults and may be at the origin of the volcanism in the massif (but the hypothesis is not proved yet). In fact, above the crystalline foundation, one can observe many volcanoes of many different types and ages: volcanic plateaus (Aubrac, Cézallier), stratovolcanoes (Mounts of Cantal, Monts Dore), and small, very recent monogenic volcanoes (Chaîne des Puys, Vivarais). The entire region contains a large concentration of around 450 extinct volcanoes. The Chaîne des Puys (near Clermont-Ferrand), a range running north to south and less than 160 km2 (60 sq mi) long, contains 115 of them (monogenic volcanoes only).[citation needed] The Auvergne Volcanoes regional natural park is in the massif. The amusement park of Vulcania near Clermont-Ferrand allows visitors to discover this natural heritage and introduces them to volcanology.

In the south, one remarkable region, made up of features called Causses in French, consists of raised limestone plateaus cut by very deep canyons. The most famous of these is the Gorges du Tarn (canyon of the Tarn).

Mountains

Mountain ranges, with notable individual mountains, are (roughly north to south):

Plateaus

Causse Méjean

Administration

The following departments are generally considered as part of the Massif Central: Allier, Ardèche, Aude, Aveyron, Cantal, Corrèze, Creuse, Gard, Haute-Garonne, Haute-Loire, Haute-Vienne, Hérault, Loire, Lot, Lozère, Puy-de-Dôme, Rhône, Saône-et-Loire, Tarn, and Tarn-et-Garonne; these form parts of the regions of Auvergne-Rhône-Alpes, Bourgogne-Franche-Comté, Nouvelle-Aquitaine and Occitania.

The largest cities in the region are Clermont-Ferrand, Limoges, and Saint-Étienne.

Economy

In the Massif Central, the industry remains little developed except locally (metallurgy in Saint-Étienne, tire industry in Clermont-Ferrand, headquarters of Michelin, world leader in the sector, aeronautics industry in Figeac, etc.). The other industries present are linked to agriculture (Groupe Limagrain, the world's third-largest seed producer, cheese-producing industries that export to the world, such as Cantal and Roquefort).

The Millau Viaduct

On the agricultural level, the Limagne plain is dominated by major cereal crops, but in the mountains, it is mainly livestock farming that predominates: cattle farming in the west for meat and milk (Cantal cheese), sheep farming in the south on the limestone plateaus (Roquefort cheese).

Finally, tourism is booming, taking advantage of the UNESCO heritage classification of the volcanoes of the Chaîne des Puys and the Causses and Cévennes region.

The entire economy of the Massif Central has benefited from the opening of roads, in particular the construction of the A75 motorway (on which is located the famous Millau Viaduct).

See also

References

  1. ^ "Massif Central" (US) and "Massif Central". Lexico UK English Dictionary. Oxford University Press. Archived from the original on 2020-03-18.
  2. ^ "Massif Central". The American Heritage Dictionary of the English Language (5th ed.). HarperCollins. Retrieved 17 May 2019.
  3. ^ "Massif Central". Merriam-Webster.com Dictionary. Retrieved 17 May 2019.
  4. ^ Occitan: Massís Central, pronounced [maˈsissenˈtɾal]; Arpitan: Massis Centrâl; literally "Central Massif"

External links

This page was last edited on 19 March 2024, at 17:49
Basis of this page is in Wikipedia. Text is available under the CC BY-SA 3.0 Unported License. Non-text media are available under their specified licenses. Wikipedia® is a registered trademark of the Wikimedia Foundation, Inc. WIKI 2 is an independent company and has no affiliation with Wikimedia Foundation.