1.
Camisard
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Camisards were Huguenots of the rugged and isolated Cévennes region, and the Vaunage in southern France. They raised an insurrection against the persecutions which followed the Revocation of the Edict of Nantes in 1685, the Camisards operated throughout the mainly protestant Cévennes region which in the eighteenth century also included the Vaunage and the parts of the Camargue around Aigues Mortes. The revolt by the Camisards broke out in 1702, with the worst of the fighting continuing until 1704, then scattered fighting until 1710, the Edict of Tolerance was not finally signed until 1787. The name camisard in the Occitan language can be attributed to a type of linen smock or shirt known as a camisa that peasants wear in lieu of any sort of uniform, alternatively, it can derive from the Occitan word camus, meaning paths. Camisada, in the sense of attack, is derived from a feature of their tactics. In April 1598, Henry IV had signed the Edict of Nantes, Protestants had been given limited civic rights and the liberty to worship according to their convictions. This fundamental and irrevocable law was maintained by Henrys son, Louis XIII, in October 1685, Henrys grandson, Louis XIV, revoked the Edict of Nantes, issuing his own Edict of Fontainebleau. Louis was determined to impose a religion on France, that of Rome. As early as 1681 he instituted the dragonnades which were enforced by dragoons. They were billeted in the homes of Protestants to help them decide to convert back to the church or alternatively to emigrate. The Cévennes was a centre of resistance, and the policy did not work, the Edict of Fontainebleau removed all rights and protections from the Huguenots. There followed about twenty years of persecutions, reformed worship and private Bible readings were outlawed. The pastors and worshippers were captured and later exiled, sent to the galleys, seventy-five missionary priests under the command of Abbot François Langlade were sent to the Cévennes. Soldiers carrying crosses on their muskets forced the peasants to sign papers to say they were converting, the peasants continued to attend illicit meeting. Huguenots with a trade, fled to neighbouring countries, the King responded by closing the borders. The Protestant peasants of the Vaunage and the Cévennes, led by a number of known as prophets, notably Franćois Vivent and Claude Brousson. Vivent encouraged his followers to arm themselves in case they were set upon by Royalist soldiers, several leading prophets were tortured and executed, Franćois Vivent in 1692 and Claude Brousson in 1698. Many more were exiled, leaving the abandoned congregations to the leadership of less educated and more mystically-oriented preachers, the Catholic church was likened to the Beast of the Apocalypse and the clandestine prophets claimed to have seen it in the prophetic dreams
2.
Occitan language
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Occitan, also known as lenga dòc by its native speakers, is a Romance language. It is spoken in southern France, Italys Occitan Valleys, Monaco, and Spains Val dAran, collectively, Occitan is also spoken in the linguistic enclave of Guardia Piemontese. However, there is controversy about the unity of the language, others include Catalan in this family, as the distance between this language and some Occitan dialects is similar to the distance among different Occitan dialects. In fact, Catalan was considered an Occitan dialect until the end of the 19th century, today, Occitan is an official language in Catalonia, where a subdialect of Gascon known as Aranese is spoken in the Val dAran. Since September 2010, the Parliament of Catalonia has considered Aranese Occitan to be the preferred language for use in the Val dAran. Unlike other Romance languages such as French or Spanish, there is no written standard language called Occitan. Instead, there are competing norms for writing Occitan, some of which attempt to be pan-dialectal, There are also significant lexical differences, where some dialects have words cognate with French, and others have Catalan and Spanish cognates. Nonetheless, there is a significant amount of mutual intelligibility, the long-term survival of Occitan is in grave doubt. According to the UNESCO Red Book of Endangered Languages, four of the six dialects of Occitan are considered severely endangered. The name Occitan comes from lenga dòc, òc being the Occitan word for yes and this was not, of course, the only defining characteristic of each group. The word òc came from Vulgar Latin hoc, while oïl originated from Latin hoc illud, Old Catalan, and now the Catalan of Northern Catalonia also have hoc. Other Romance languages derive their word for yes from the Latin sic, thus, etc. such as Spanish sí, Eastern Lombard sé, Sicilian and Italian sì, or Portuguese sim. French uses si to answer yes in response to questions that are asked in the negative sense, the name Occitan is sometimes considered a neologism, however, it was attested around 1300 as occitanus, a crossing of oc and aquitanus. For many centuries, the Occitan dialects were referred to as Limousin or Provençal, after Frédéric Mistrals Félibrige movement in the 19th century, Provençal achieved the greatest literary recognition and so became the most popular term for Occitan. The term first came into fashion in Italy, currently, linguists use the terms Provençal and Limousin strictly to refer to specific varieties within Occitania, keeping the name Occitan for the language as a whole. Many non-specialists, however, continue to refer to the language as Provençal, NO·L LI TOLRÀ NO·L LI DEVEDARÀ NI NO LEN DECEBRÀ. Nec societatem non AURÀ, si per castellum recuperare NON O FA, et si recuperare potuerit in potestate Froterio et Raimundo LO TORNARÀ, carolingian litanies, both written and sung in Latin, were answered to in Old Occitan by the audience. Occitan was the vehicle for the poetry of the medieval troubadours and trobairises, At that time
3.
Gorges du Tarn
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The Gorges du Tarn is a canyon formed by the Tarn River between the Causse Méjean and the Causse de Sauveterre, in southern France. The canyon, mainly located in the Lozère département, and partially in the Aveyron département, is about 53 kilometres -long and 400 m to 600 m deep, the architecture of the gorges involves Mesozoic limestone plateaux downstream presenting sub-vertical cliffs. Faults like the Hauterive Fault explain the important water sources in the region of Sainte-Enimie, the climate is Mediterranean, with relatively mild winters and very warm summers. Tourism in Tarn Office de Tourisme des Cévennes - Gorges du Tarn Gorges du Tarn on About-France. com
4.
Summit
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A summit is a point on a surface that is higher in elevation than all points immediately adjacent to it. Mathematically, a summit is a maximum in elevation. The topographic terms acme, apex, peak, and zenith are synonymous, the UIAA definition is that a summit is independent if it has a prominence of 30 metres or more, it is a mountain if it has a prominence of at least 300 metres. This can be summarised as follows, A pyramidal peak is an exaggerated form produced by ice erosion of a mountain top, Summit may also refer to the highest point along a line, trail, or route. In many parts of the western United States, the term refers to the highest point along a road, highway. For example, the highest point along Interstate 80 in California is referred to as Donner Summit while the highest point on Interstate 5 is Siskiyou Mountain Summit, geoid Hill List of highest mountains Maxima and minima Nadir Summit accordance Peak finder
5.
Geographic coordinate system
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A geographic coordinate system is a coordinate system used in geography that enables every location on Earth to be specified by a set of numbers, letters or symbols. The coordinates are chosen such that one of the numbers represents a vertical position. A common choice of coordinates is latitude, longitude and elevation, to specify a location on a two-dimensional map requires a map projection. The invention of a coordinate system is generally credited to Eratosthenes of Cyrene. Ptolemy credited him with the adoption of longitude and latitude. Ptolemys 2nd-century Geography used the prime meridian but measured latitude from the equator instead. Mathematical cartography resumed in Europe following Maximus Planudes recovery of Ptolemys text a little before 1300, in 1884, the United States hosted the International Meridian Conference, attended by representatives from twenty-five nations. Twenty-two of them agreed to adopt the longitude of the Royal Observatory in Greenwich, the Dominican Republic voted against the motion, while France and Brazil abstained. France adopted Greenwich Mean Time in place of local determinations by the Paris Observatory in 1911, the latitude of a point on Earths surface is the angle between the equatorial plane and the straight line that passes through that point and through the center of the Earth. Lines joining points of the same latitude trace circles on the surface of Earth called parallels, as they are parallel to the equator, the north pole is 90° N, the south pole is 90° S. The 0° parallel of latitude is designated the equator, the plane of all geographic coordinate systems. The equator divides the globe into Northern and Southern Hemispheres, the longitude of a point on Earths surface is the angle east or west of a reference meridian to another meridian that passes through that point. All meridians are halves of great ellipses, which converge at the north and south poles, the prime meridian determines the proper Eastern and Western Hemispheres, although maps often divide these hemispheres further west in order to keep the Old World on a single side. The antipodal meridian of Greenwich is both 180°W and 180°E, the combination of these two components specifies the position of any location on the surface of Earth, without consideration of altitude or depth. The grid formed by lines of latitude and longitude is known as a graticule, the origin/zero point of this system is located in the Gulf of Guinea about 625 km south of Tema, Ghana. To completely specify a location of a feature on, in, or above Earth. Earth is not a sphere, but a shape approximating a biaxial ellipsoid. It is nearly spherical, but has an equatorial bulge making the radius at the equator about 0. 3% larger than the radius measured through the poles, the shorter axis approximately coincides with the axis of rotation
6.
Massif Central
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The Massif Central is an elevated region in the middle of southern France, consisting of mountains and plateaus. It covers approximately 15 percent of the country, 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 up the Massif Central itself. The Massif Central is an old massif, formed during the Variscan orogeny and 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. These tectonic movements created faults and are maybe at the origin of the volcanism in the Massif Central, in fact, above the crystalline foundation, we can observe many volcanoes of many different types and ages, volcanic plateaus, stratovolcanoes, and small, very recent monogenic volcanoes. The entire region contains a concentration of approximately 450 extinct volcanoes. The strip of Chaîne des Puys, running north to south and less than 60 square miles long, the Auvergne Volcanoes National Park is in the massif. In the south, one region, made up of features called causses in French. The most famous of these is the canyon of Tarn, the following régions are part of the Massif Central, Auvergne, Limousin. Part of the following régions are in the Massif Central, Languedoc-Roussillon, the largest cities are Clermont-Ferrand and Saint-Étienne
7.
France
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France, officially the French Republic, is a country with territory in western Europe and several overseas regions and territories. The European, or metropolitan, area of France extends from the Mediterranean Sea to the English Channel and the North Sea, Overseas France include French Guiana on the South American continent and several island territories in the Atlantic, Pacific and Indian oceans. France spans 643,801 square kilometres and had a population of almost 67 million people as of January 2017. It is a unitary republic with the capital in Paris. Other major urban centres include Marseille, Lyon, Lille, Nice, Toulouse, during the Iron Age, what is now metropolitan France was inhabited by the Gauls, a Celtic people. The area was annexed in 51 BC by Rome, which held Gaul until 486, France emerged as a major European power in the Late Middle Ages, with its victory in the Hundred Years War strengthening state-building and political centralisation. During the Renaissance, French culture flourished and a colonial empire was established. The 16th century was dominated by civil wars between Catholics and Protestants. France became Europes dominant cultural, political, and military power under Louis XIV, in the 19th century Napoleon took power and established the First French Empire, whose subsequent Napoleonic Wars shaped the course of continental Europe. Following the collapse of the Empire, France endured a succession of governments culminating with the establishment of the French Third Republic in 1870. Following liberation in 1944, a Fourth Republic was established and later dissolved in the course of the Algerian War, the Fifth Republic, led by Charles de Gaulle, was formed in 1958 and remains to this day. Algeria and nearly all the colonies became independent in the 1960s with minimal controversy and typically retained close economic. France has long been a centre of art, science. It hosts Europes fourth-largest number of cultural UNESCO World Heritage Sites and receives around 83 million foreign tourists annually, France is a developed country with the worlds sixth-largest economy by nominal GDP and ninth-largest by purchasing power parity. In terms of household wealth, it ranks fourth in the world. France performs well in international rankings of education, health care, life expectancy, France remains a great power in the world, being one of the five permanent members of the United Nations Security Council with the power to veto and an official nuclear-weapon state. It is a member state of the European Union and the Eurozone. It is also a member of the Group of 7, North Atlantic Treaty Organization, Organisation for Economic Co-operation and Development, the World Trade Organization, originally applied to the whole Frankish Empire, the name France comes from the Latin Francia, or country of the Franks
8.
Departments of France
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In the administrative divisions of France, the department is one of the three levels of government below the national level, between the administrative regions and the commune. There are 96 departments in metropolitan France and 5 overseas departments, each department is administered by an elected body called a departmental council. From 1800 to April 2015, they were called general councils, the departments were created in 1791 as a rational replacement of Ancien Régime provinces with a view to strengthen national unity, the title department is used to mean a part of a larger whole. Almost all of them were named after geographical features rather than after historical or cultural territories which could have their own loyalties. The earliest known suggestion of it is from 1764 in the writings of dArgenson and they have inspired similar divisions in many countries, some of them former French colonies. Most French departments are assigned a number, the Official Geographical Code. Some overseas departments have a three-digit number, the number is used, for example, in the postal code, and was until recently used for all vehicle registration plates. For example, inhabitants of Loiret might refer to their department as the 45 and this reform project has since been abandoned. The first French territorial departments were proposed in 1665 by Marc-René dArgenson to serve as administrative areas purely for the Ponts et Chaussées infrastructure administration, before the French Revolution, France gained territory gradually through the annexation of a mosaic of independent entities. By the close of the Ancien Régime, it was organised into provinces, during the period of the Revolution, these were dissolved, partly in order to weaken old loyalties. Their boundaries served two purposes, Boundaries were chosen to break up Frances historical regions in an attempt to erase cultural differences, Boundaries were set so that every settlement in the country was within a days ride of the capital of the department. This was a security measure, intended to keep the national territory under close control. This measure was directly inspired by the Great Terror, during which the government had lost control of rural areas far from any centre of government. The old nomenclature was carefully avoided in naming the new departments, most were named after an areas principal river or other physical features. Even Paris was in the department of Seine, the number of departments, initially 83, was increased to 130 by 1809 with the territorial gains of the Republic and of the First French Empire. Following Napoleons defeats in 1814-1815, the Congress of Vienna returned France to its pre-war size, in 1860, France acquired the County of Nice and Savoy, which led to the creation of three new departments. Two were added from the new Savoyard territory, while the department of Alpes-Maritimes was created from Nice, the 89 departments were given numbers based on their alphabetical order. The department of Bas-Rhin and parts of Meurthe, Moselle, Vosges and Haut-Rhin were ceded to the German Empire in 1871, following Frances defeat in the Franco-Prussian War
9.
Mountain range
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A mountain range is a geographic area containing numerous geologically related mountains. A mountain system or system of ranges, sometimes is used to combine several geological features that are geographically related. Mountain ranges are usually segmented by highlands or mountain passes and valleys, individual mountains within the same mountain range do not necessarily have the same geologic structure or petrology. They may be a mix of different orogenic expressions and terranes, for example thrust sheets, uplifted blocks, fold mountains, most geologically young mountain ranges on the Earths land surface are associated with either the Pacific Ring of Fire or the Alpide Belt. The Andes is 7,000 kilometres long and is considered the worlds longest mountain system. The Alpide belt includes Indonesia and southeast Asia, through the Himalaya, the belt also includes other European and Asian mountain ranges. The Himalayas contain the highest mountains in the world, including Mount Everest, mountain ranges outside of these two systems include the Arctic Cordillera, the Urals, the Appalachians, the Scandinavian Mountains, the Altai Mountains and the Hijaz Mountains. If the definition of a range is stretched to include underwater mountains. The mountain systems of the earth are characterized by a tree structure, the sub-range relationship is often expressed as a parent-child relationship. For example, the White Mountains of New Hampshire and the Blue Ridge Mountains are sub-ranges of the Appalachian Mountains, equivalently, the Appalachians are the parent of the White Mountains and Blue Ridge Mountains, and the White Mountains and the Blue Ridge Mountains are children of the Appalachians. The position of mountains influences climate, such as rain or snow, when air masses move up and over mountains, the air cools producing orographic precipitation. As the air descends on the side, it warms again and is drier. Often, a shadow will affect the leeward side of a range. Mountain ranges are constantly subjected to forces which work to tear them down. Erosion is at work while the mountains are being uplifted and long after until the mountains are reduced to low hills, rivers are traditionally believed to be the principle erosive factor on mountain ranges, with their ability of bedrock incision and sediment transport. The rugged topography of a range is the product of erosion. The basins adjacent to a mountain range are filled with sediments which are buried and turned into sedimentary rock. The early Cenozoic uplift of the Rocky Mountains of Colorado provides an example and this mass of rock was removed as the range was actively undergoing uplift
