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Montdardier
Montdardier (; oc, Montdardièr) is a commune in the Gard department in southern France. Geography Climate Montdardier has a warm-summer Mediterranean climate (Köppen climate classification ''Csb'') closely bordering on a hot-summer Mediterranean climate (''Csa''). The average annual temperature in Montdardier is . The average annual rainfall is with October as the wettest month. The temperatures are highest on average in July, at around , and lowest in January, at around . The highest temperature ever recorded in Montdardier was on 28 June 2019; the coldest temperature ever recorded was on 27 February 2018. Population Sights *The castle in neo-gothic style *''La Tude massif'' *The church Several quarries above Montdardier were formerly important sources of lithographic limestone. Stone from these quarries, marketed as Vigan stone, earned an honorable mention in the Great Exhibition of 1851.Class I, Report on Mining, Quarrying, Metallurgical Operations, and Mineral ...
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Montdardier Chateau Carte
Montdardier (; oc, Montdardièr) is a Communes of France, commune in the Gard Departments of France, department in southern France. Geography Climate Montdardier has a warm-summer Mediterranean climate (Köppen climate classification ''Csb'') closely bordering on a hot-summer Mediterranean climate (''Csa''). The average annual temperature in Montdardier is . The average annual rainfall is with October as the wettest month. The temperatures are highest on average in July, at around , and lowest in January, at around . The highest temperature ever recorded in Montdardier was on 28 June 2019; the coldest temperature ever recorded was on 27 February 2018. Population Sights *The castle in neo-gothic style *''La Tude massif'' *The church Several quarry, quarries above Montdardier were formerly important sources of lithographic limestone. Stone from these quarries, marketed as le Vigan, Gard, Vigan stone, earned an honorable mention in the Great Exhibition of 1851.Class I, Re ...
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Lithographic Limestone
Lithographic limestone is hard limestone that is sufficiently fine-grained, homogeneous and defect free to be used for lithography. Geologists use the term "lithographic texture" to refer to a grain size under 1/250 mm. The term "sublithographic" is sometimes used for homogeneous fine-grained limestone with a somewhat coarser texture. Origin The generally accepted theory for the origin of lithographic and sublithographic limestones is that they were formed in shallow, stagnant, hypersaline, and anoxic lagoons. The combination of mild hypersalinity and low oxygen content is believed to have inhibited the formation of microbial mats and prevented the invasion of bottom dwelling organisms. Microbial mats and bottom dwelling organisms would have left fossils, and bottom dwelling organisms would have churned the accumulating sediment, producing a less homogeneous rock. Stagnancy was required to avoid churning or sculpting of the sediment by currents or wave action.Walter E ...
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Le Vigan, Gard
Le Vigan (; oc, Lo Vigan) is a commune in the Gard department in southern France. It is a sub-prefecture of the department. Geography Le Vigan is located at the south of the Massif Central and near the Mont Aigoual, in the Arre valley. The town is on the southern edge of the Cévennes National Park and is the most populous town within the park. Climate Le Vigan has a hot-summer Mediterranean climate (Köppen climate classification ''Csa''). The average annual temperature in Le Vigan is . The average annual rainfall is with October as the wettest month. The temperatures are highest on average in July, at around , and lowest in January, at around . The highest temperature ever recorded in Le Vigan was on 28 June 2019; the coldest temperature ever recorded was on 16 January 1985. History On a river at the southern edge of the Massif Central, Le Vigan is situated on a natural boundaryline. In the 2nd-3rd centuries BCE, it was situated between the territories occupied b ...
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Communes Of The Gard Department
This is a list of the 351 communes of the Gard department of France. The communes cooperate in the following intercommunalities (as of 2020):BANATIC
Périmètre des EPCI à fiscalité propre. Accessed 3 July 2020.
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Causse De Blandas
Causse de Blandas is a limestone karst plateau in the south of the Massif Central in the Gard department, in southern France. Geography The communes of causse de Blandas are: * Blandas *Montdardier *Rogues See also * Causses * cirque de Navacelles * Vis river The Vis is a river in south-central France, in the Occitanie administrative region. It is a right tributary of the Hérault. Its source is in the Cévennes, near the village of Alzon. It flows between the Causse du Larzac and the Causse ... Landforms of Gard Plateaus of Metropolitan France {{Gard-geo-stub ...
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Communes Of France
The () is a level of administrative division in the French Republic. French are analogous to civil townships and incorporated municipalities in the United States and Canada, ' in Germany, ' in Italy, or ' in Spain. The United Kingdom's equivalent are civil parishes, although some areas, particularly urban areas, are unparished. are based on historical geographic communities or villages and are vested with significant powers to manage the populations and land of the geographic area covered. The are the fourth-level administrative divisions of France. vary widely in size and area, from large sprawling cities with millions of inhabitants like Paris, to small hamlets with only a handful of inhabitants. typically are based on pre-existing villages and facilitate local governance. All have names, but not all named geographic areas or groups of people residing together are ( or ), the difference residing in the lack of administrative powers. Except for the municipal arr ...
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Village Montdardier
A village is a clustered human settlement or Residential community, community, larger than a hamlet (place), hamlet but smaller than a town (although the word is often used to describe both hamlets and smaller towns), with a population typically ranging from a few hundred to a few thousand. Though villages are often located in rural areas, the term urban village is also applied to certain urban neighborhoods. Villages are normally permanent, with fixed dwellings; however, transient villages can occur. Further, the dwellings of a village are fairly close to one another, not scattered broadly over the landscape, as a dispersed settlement. In the past, villages were a usual form of community for societies that practice subsistence agriculture, and also for some non-agricultural societies. In Great Britain, a hamlet earned the right to be called a village when it built a Church (building), church.
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Gard
Gard () is a department in Southern France, located in the region of Occitanie. It had a population of 748,437 as of 2019;Populations légales 2019: 30 Gard
INSEE
its is . The department is named after the river Gardon; the Occitan name of the river, Gard (), has been replacing the French name in recent decades, both administratively and among French speakers. < ...
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Departments Of France
In the administrative divisions of France, the department (french: département, ) is one of the three levels of government under the national level ("territorial collectivities"), between the administrative regions and the communes. Ninety-six departments are in metropolitan France, and five are overseas departments, which are also classified as overseas regions. Departments are further subdivided into 332 arrondissements, and these are divided into cantons. The last two levels of government have no autonomy; they are the basis of local organisation of police, fire departments and, sometimes, administration of elections. Each department is administered by an elected body called a departmental council ( ing. lur.. From 1800 to April 2015, these were called general councils ( ing. lur.. Each council has a president. Their main areas of responsibility include the management of a number of social and welfare allowances, of junior high school () buildings and technical ...
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France
France (), officially the French Republic ( ), is a country primarily located in Western Europe. It also comprises of overseas regions and territories in the Americas and the Atlantic, Pacific and Indian Oceans. Its metropolitan area extends from the Rhine to the Atlantic Ocean and from the Mediterranean Sea to the English Channel and the North Sea; overseas territories include French Guiana in South America, Saint Pierre and Miquelon in the North Atlantic, the French West Indies, and many islands in Oceania and the Indian Ocean. Due to its several coastal territories, France has the largest exclusive economic zone in the world. France borders Belgium, Luxembourg, Germany, Switzerland, Monaco, Italy, Andorra, and Spain in continental Europe, as well as the Netherlands, Suriname, and Brazil in the Americas via its overseas territories in French Guiana and Saint Martin. Its eighteen integral regions (five of which are overseas) span a combined area of ...
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Warm-summer Mediterranean Climate
A Mediterranean climate (also called a dry summer temperate climate ''Cs'') is a temperate climate sub-type, generally characterized by warm, dry summers and mild, fairly wet winters; these weather conditions are typically experienced in the majority of Mediterranean-climate regions and countries, but remain highly dependent on proximity to the ocean, altitude and geographical location. This climate type's name is in reference to the coastal regions of the Mediterranean Sea within the Mediterranean Basin, where this climate type is most prevalent. The "original" Mediterranean zone is a massive area, its western region beginning with the Iberian Peninsula in southwestern Europe and coastal regions of northern Morocco, extending eastwards across southern Europe, the Balkans, and coastal Northern Africa, before reaching a dead-end at the Levant region's coastline. Mediterranean climate zones are typically located along the western coasts of landmasses, between roughly 30 and 4 ...
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Köppen Climate Classification
The Köppen climate classification is one of the most widely used climate classification systems. It was first published by German-Russian climatologist Wladimir Köppen (1846–1940) in 1884, with several later modifications by Köppen, notably in 1918 and 1936. Later, the climatologist Rudolf Geiger (1894–1981) introduced some changes to the classification system, which is thus sometimes called the Köppen–Geiger climate classification system. The Köppen climate classification divides climates into five main climate groups, with each group being divided based on seasonal precipitation and temperature patterns. The five main groups are ''A'' (tropical), ''B'' (arid), ''C'' (temperate), ''D'' (continental), and ''E'' (polar). Each group and subgroup is represented by a letter. All climates are assigned a main group (the first letter). All climates except for those in the ''E'' group are assigned a seasonal precipitation subgroup (the second letter). For example, ''Af'' i ...
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