1.
Marne (river)
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The Marne is a river in France, an eastern tributary of the Seine in the area east and southeast of Paris. The river gave its name to the départements of Haute-Marne, Marne, Seine-et-Marne, the Marne starts in the Langres plateau, runs generally north then bends west between Saint-Dizier and Châlons-en-Champagne, joining the Seine at Charenton just upstream from Paris. Its main tributaries are the Rognon, the Blaise, the Saulx, the Ourcq, the Petit Morin, in the Champagne région, part of the water is led through the artificial lake Lac du Der-Chantecoq, in order to regulate the water discharge. This way, large inundations or low river levels downstream are prevented, the Celts of Gaul worshipped a goddess known as Dea Matrona who was associated with the Marne. The Marne is famous as the site of the two battles during the First World War. The first battle was a point of World War I. The second battle was fought four years later, in 1918, during the heyday of canal transportation, the Marne was a major artery connecting Paris and the Seine with major rivers nearby such as the Meuse, the Moselle and the Rhine, and the Saône and Rhône. To facilitate transportation along the Marne itself, a number of canals were constructed alongside. The most extensive was the Canal latéral à la Marne, which runs 67 km between Vitry-le-François and Dizy, river Marne guide Places, ports and moorings on the river
2.
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
3.
Prefectures in France
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There are 101 prefectures in France, one for each department. The official in charge is the prefect, the prefect represents the national government at the local level and as such exercises the powers that are constitutionally attributed to the national government. The prefect issues ordinances written for the application of law, to close a building that does not conform to safety codes. In the past, the prefect was head of the department, but since 1982, there is an exception in Paris and its three surrounding departments. These departments are administered by a prefecture for law enforcement and security purposes, called the Prefecture of Police. The power of law enforcement is usually invested in the mayor in other French communes, the departments are divided into arrondissements, themselves divided into cantons. The chef-lieu darrondissement is the subprefecture, the official in charge is the subprefect (French, sous-préfet. Cantons have relatively few competences, the most important one being the local organisation of elections, administrative divisions of France French National Police
4.
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
5.
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
6.
Regions of France
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France is divided into 18 administrative regions, including 13 metropolitan regions and 5 overseas regions. The current legal concept of region was adopted in 1982, the term région was officially created by the Law of Decentralisation, which also gave regions their legal status. The first direct elections for representatives took place on 16 March 1986. In 2016, the number of regions was reduced from 27 to 18 through amalgamation, in 2014, the French parliament passed a law reducing the number of metropolitan regions from 22 to 13 with effect from 1 January 2016. However, the region of Upper and Lower Normandy is simply called Normandy. Permanent names were to be proposed by the new regional councils by 1 July 2016, the legislation defining the new regions also allowed the Centre region to officially change its name to Centre-Val de Loire with effect from January 2015. Two regions, Auvergne-Rhône-Alpes and Bourgogne-Franche-Comté, opted to retain their interim names, between 1982 and 2015, there were 22 regions in Metropolitan France. Before 2011, there were four regions, in 2011 Mayotte became the fifth. Regions lack separate legislative authority and therefore cannot write their own statutory law and they levy their own taxes and, in return, receive a decreasing part of their budget from the central government, which gives them a portion of the taxes it levies. They also have considerable budgets managed by a council made up of representatives voted into office in regional elections. A regions primary responsibility is to build and furnish high schools, in March 2004, the French central government unveiled a controversial plan to transfer regulation of certain categories of non-teaching school staff to the regional authorities. Critics of this plan contended that tax revenue was insufficient to pay for the costs. In addition, regions have considerable power over infrastructural spending, e. g. education, public transit, universities and research. This has meant that the heads of regions such as Île-de-France or Rhône-Alpes can be high-profile positions. Number of regions controlled by each coalition since 1986, Overseas region is a recent designation, given to the overseas departments that have similar powers to those of the regions of metropolitan France. Radio France Internationale in English Overseas regions Ministère de lOutre-Mer some explanations about the past and current developments of DOMs and TOMs
7.
Subprefectures in France
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In France, a subprefecture is the administrative center of a departmental arrondissement that does not contain the prefecture for its department. The term also applies to the building houses the administrative headquarters for an arrondissement. The civil servant in charge of a subprefecture is the subprefect, between May 1982 and February 1988, subprefects were known instead by the title commissaire adjoint de la République. Where the administration of an arrondissement is carried out from a prefecture, the municipal arrondissements of Paris, Lyon, and Marseille) are divisions of the city rather than the prefecture, and so are not arrondissements in the same sense
8.
Reims
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Reims, a city in the Grand Est region of France, lies 129 km east-northeast of Paris. The 2013 census recorded 182,592 inhabitants in the city of Reims proper and its river, the Vesle, is a tributary of the Aisne. Founded by the Gauls, it became a city during the period of the Roman Empire. Reims played a prominent ceremonial role in French monarchical history as the site of the crowning of the kings of France. The Cathedral of Reims housed the Holy Ampulla containing the Saint Chrême and it was used for the anointing, the most important part of the coronation of French kings. Reims functions as a subprefecture of the department of Marne, in the region of Grand Est. Although Reims is by far the largest commune in both its region and department, Châlons-en-Champagne is the capital and prefecture of both. Before the Roman conquest of northern Gaul, Reims, founded circa 80 BC as *Durocorteron, at its height in Roman times the city had a population in the range of 30,000 -50,000 or perhaps up to 100,000. Christianity had become established in the city by 260, at which period Saint Sixtus of Reims founded the bishopric of Reims, for centuries the events at the crowning of Clovis I became a symbol used by the monarchy to claim the divine right to rule. Meetings of Pope Stephen II with Pepin the Short, and of Pope Leo III with Charlemagne, took place at Reims, Louis IV gave the city and countship of Reims to the archbishop Artaldus in 940. Louis VII gave the title of duke and peer to William of Champagne, archbishop from 1176 to 1202, by the 10th century Reims had become a centre of intellectual culture. Archbishop Adalberon, seconded by the monk Gerbert, founded schools which taught the liberal arts. Louis XI cruelly suppressed a revolt at Reims, caused in 1461 by the salt tax, during the French Wars of Religion the city sided with the Catholic League, but submitted to Henri IV after the battle of Ivry. In August 1909 Reims hosted the first international meet, the Grande Semaine dAviation de la Champagne. Major aviation personages such as Glenn Curtiss, Louis Blériot and Louis Paulhan participated, hostilities in World War I greatly damaged the city. German bombardment and a subsequent fire in 1914 did severe damage to the cathedral, from the end of World War I to the present day an international effort to restore the cathedral from the ruins has continued. The Palace of Tau, St Jacques Church and the Abbey of St Remi also were protected and restored, the collection of preserved buildings and Roman ruins remains monumentally impressive. During World War II the city suffered additional damage, but in Reims, at 2,41 on the morning of 7 May 1945, General Eisenhower and the Allies received the unconditional surrender of the German Wehrmacht
9.
List of French departments by population
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This table lists the 101 French departments in descending order of population, area and population density. The figures include, population without double counting for 1999, municipal population published in decree No, 2010-1723 of 30 December 2010 as amended by Decree No. 2011-343 of 28 March 2011 which corresponds to data compiled as at 1 January 2008, municipal population The total population takes into account double counting. Guadeloupe has seemingly lost population between 1999 and 2008, however, this diminution of the legal population is due to the creation of the overseas communities of Saint Barthelemy and Saint-Martin. In the 1999 census, the population of Guadeloupe without the arrondissement of Saint-Martin-Saint-Barthélemy was 386,566 inhabitants, the departments population has actually increased by more than 15,000 people over the period based on a constant territory
10.
Daylight saving time
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Daylight saving time is the practice of advancing clocks during summer months by one hour so that evening daylight lasts an hour longer, while sacrificing normal sunrise times. Typically, regions that use Daylight Savings Time adjust clocks forward one hour close to the start of spring, American inventor and politician Benjamin Franklin proposed a form of daylight time in 1784. New Zealander George Hudson proposed the idea of saving in 1895. The German Empire and Austria-Hungary organized the first nationwide implementation, starting on April 30,1916, many countries have used it at various times since then, particularly since the energy crisis of the 1970s. The practice has both advocates and critics, DST clock shifts sometimes complicate timekeeping and can disrupt travel, billing, record keeping, medical devices, heavy equipment, and sleep patterns. Computer software often adjusts clocks automatically, but policy changes by various jurisdictions of DST dates, industrialized societies generally follow a clock-based schedule for daily activities that do not change throughout the course of the year. The time of day that individuals begin and end work or school, North and south of the tropics daylight lasts longer in summer and shorter in winter, with the effect becoming greater as one moves away from the tropics. However, they will have one hour of daylight at the start of each day. Supporters have also argued that DST decreases energy consumption by reducing the need for lighting and heating, DST is also of little use for locations near the equator, because these regions see only a small variation in daylight in the course of the year. After ancient times, equal-length civil hours eventually supplanted unequal, so civil time no longer varies by season, unequal hours are still used in a few traditional settings, such as some monasteries of Mount Athos and all Jewish ceremonies. This 1784 satire proposed taxing window shutters, rationing candles, and waking the public by ringing church bells, despite common misconception, Franklin did not actually propose DST, 18th-century Europe did not even keep precise schedules. However, this changed as rail transport and communication networks came to require a standardization of time unknown in Franklins day. Modern DST was first proposed by the New Zealand entomologist George Hudson, whose shift work job gave him time to collect insects. An avid golfer, he also disliked cutting short his round at dusk and his solution was to advance the clock during the summer months, a proposal he published two years later. The proposal was taken up by the Liberal Member of Parliament Robert Pearce, a select committee was set up to examine the issue, but Pearces bill did not become law, and several other bills failed in the following years. Willett lobbied for the proposal in the UK until his death in 1915, william Sword Frost, mayor of Orillia, Ontario, introduced daylight saving time in the municipality during his tenure from 1911 to 1912. Starting on April 30,1916, the German Empire and its World War I ally Austria-Hungary were the first to use DST as a way to conserve coal during wartime, Britain, most of its allies, and many European neutrals soon followed suit. Russia and a few other countries waited until the year
11.
Central European Summer Time
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It corresponds to UTC + two hours. Other names which have been applied to Central European Summer Time are Middle European Summer Time, Central European Daylight Saving Time, and Bravo Time. Since 1996 European Summer Time has been observed between 1,00 UTC on the last Sunday of March and 1,00 on the last Sunday of October, the following countries and territories use Central European Summer Time. In addition, Libya used CEST during the years 1951–1959, 1982–1989, 1996–1997, European Summer Time Other countries and territories in UTC+2 time zone Other names of UTC+2 time zone
12.
Communes in France
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The commune is a level of administrative division in the French Republic. French communes are roughly equivalent to civil townships incorporated municipalities in the United States or Gemeinden in Germany, the United Kingdom has no exact equivalent, as communes resemble districts in urban areas, but are closer to parishes in rural areas where districts are much larger. Communes are based on historical geographic communities or villages and have received significant powers of governance to manage the populations, the communes are the fourth-level administrative divisions of France. A French commune may be a city of 2.2 million inhabitants like Paris, communes typically are based on pre-existing villages and facilitate local governance. All communes have names, but not all named geographic areas or groups of people residing together are communes, a commune is a town, city, or municipality. Use of commune in English is a habit, and one that might be corrected. There is nothing in commune in French that is different from town in English. The French word commune appeared in the 12th century, from Medieval Latin communia, as of January 2015, there were 36,681 communes in France,36,552 of them in metropolitan France and 129 of them overseas. This is a higher total than that of any other European country. The whole territory of the French Republic is divided into communes and this is unlike some other countries, such as the United States, where unincorporated areas directly governed by a county or a higher authority can be found. There are only a few exceptions, COM of Saint-Martin and it was previously a commune inside the Guadeloupe région. The commune structure was abolished when Saint-Martin became an overseas collectivity on 22 February 2007, COM of Wallis and Futuna, which still is divided according to the three traditional chiefdoms. It was previously a commune inside the Guadeloupe region, the commune structure was abolished when Saint-Barthélemy became an overseas collectivity on 22 February 2007.88 square kilometres. The median area of metropolitan Frances communes at the 1999 census was even smaller, the median area is a better measure of the area of a typical French commune. This median area is smaller than that of most European countries. In Italy, the area of communes is 22 km2, in Belgium it is 40 km2, in Spain it is 35 km2, and in Germany. Switzerland and the Länder of Rhineland-Palatinate, Schleswig-Holstein, and Thuringia in Germany were the places in Europe where the communes had a smaller median area than in France. The communes of Frances overseas départements such as Réunion and French Guiana are large by French standards and they usually group into the same commune several villages or towns, often with sizeable distances among them
13.
Estuary
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An estuary is a partially enclosed coastal body of brackish water with one or more rivers or streams flowing into it, and with a free connection to the open sea. Estuaries form a zone between river environments and maritime environments. They are subject both to marine influences—such as tides, waves, and the influx of saline water—and to riverine influences—such as flows of fresh water and sediment. The inflows of sea water and fresh water provide high levels of nutrients both in the water column and in sediment, making estuaries among the most productive natural habitats in the world. Most existing estuaries formed during the Holocene epoch with the flooding of river-eroded or glacially scoured valleys when the sea began to rise about 10. Estuaries are typically classified according to their geomorphological features or to water-circulation patterns, the banks of many estuaries are amongst the most heavily populated areas of the world, with about 60% of the worlds population living along estuaries and the coast. The word estuary is derived from the Latin word aestuarium meaning tidal inlet of the sea, there have been many definitions proposed to describe an estuary. However, this definition excludes a number of water bodies such as coastal lagoons. This broad definition also includes fjords, lagoons, river mouths, an estuary is a dynamic ecosystem having a connection to the open sea through which the sea water enters with the rhythm of the tides. The sea water entering the estuary is diluted by the water flowing from rivers. The pattern of dilution varies between different estuaries and depends on the volume of water, the tidal range. Drowned river valleys are known as coastal plain estuaries. In places where the sea level is rising relative to the land, sea water progressively penetrates into river valleys and this is the most common type of estuary in temperate climates. Well-studied estuaries include the Severn Estuary in the United Kingdom and the Ems Dollard along the Dutch-German border, the width-to-depth ratio of these estuaries is typically large, appearing wedge-shaped in the inner part and broadening and deepening seaward. Water depths rarely exceed 30 m, examples of this type of estuary in the U. S. are the Hudson River, Chesapeake Bay, and Delaware Bay along the Mid-Atlantic coast, and Galveston Bay and Tampa Bay along the Gulf Coast. They are relatively common in tropical and subtropical locations and these estuaries are semi-isolated from ocean waters by barrier beaches. Formation of barrier beaches partially encloses the estuary, with only narrow inlets allowing contact with the ocean waters, bar-built estuaries typically develop on gently sloping plains located along tectonically stable edges of continents and marginal sea coasts. They are extensive along the Atlantic and Gulf coasts of the U. S. in areas with active coastal deposition of sediments, barrier beaches form in shallow water and are generally parallel to the shoreline, resulting in long, narrow estuaries
14.
Champagne
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The primary grapes used in the production of Champagne are black Pinot noir and Pinot Meunier but also white Chardonnay. Champagne appellation law only allows grapes grown according to rules in specifically designated plots within the appellation to be used in the production of champagne. Royalty became associated with Champagne in the 17th, 18th, the leading manufacturers made efforts to associate their Champagnes with nobility and royalty through advertising and packaging, which led to popularity among the emerging middle class. Patricia Harmsworth, Viscountess Rothermere, the English socialite, was nicknamed Bubbles after her love of champagne, wines from the Champagne region were known before medieval times. The Romans were the first to plant vineyards in this area of north-east France, with the region being cultivated by at least the 5th century, later, churches owned vineyards and monks produced wine for use in the sacrament of Eucharist. French kings were anointed in Reims, and Champagne was served as part of coronation festivities. The Champenois were envious of the reputation of the wines made by their Burgundian neighbours to the south, however, the northerly climate of the region gave the Champenois a unique set of challenges in making red wine. At the far extremes of sustainable viticulture, the grapes would struggle to fully and often would have bracing levels of acidity. The wines would be lighter bodied and thinner than the Burgundy wines they were seeking to outdo, the oldest recorded sparkling wine is Blanquette de Limoux, which was apparently invented by Benedictine Monks in the Abbey of Saint-Hilaire, near Carcassonne in 1531. They achieved this by bottling the wine before the initial fermentation had ended, Merret presented a paper at the Royal Society, in which he detailed what is now called méthode champenoise, in 1662. French glass-makers at this time could not produce bottles of the quality or strength. As early as 1663 the poet Samuel Butler referred to brisk champagne, in France the first sparkling Champagne was created accidentally, the pressure in the bottle led it to be called the devils wine, as bottles exploded or corks popped. In 1844 Adolphe Jaquesson invented the muselet to prevent the corks from blowing out, initial versions were difficult to apply and inconvenient to remove. Even when it was produced as a sparkling wine, Champagne was for a very long time made by the méthode rurale. Champagne did not use the méthode champenoise until the 19th century, the 19th century saw an exponential growth in Champagne production, going from a regional production of 300,000 bottles a year in 1800 to 20 million bottles in 1850. In 2007, Champagne sales hit a record of 338.7 million bottles. In the 19th century Champagne was noticeably sweeter than the Champagnes of today, the trend towards drier Champagne began when Perrier-Jouët decided not to sweeten his 1846 vintage prior to exporting it to London. The designation Brut Champagne was created for the British in 1876 and they include codification of the most suitable growing places, the most suitable grape types, and a lengthy set of requirements specifying most aspects of viticulture
15.
French Revolution
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Through the Revolutionary Wars, it unleashed a wave of global conflicts that extended from the Caribbean to the Middle East. Historians widely regard the Revolution as one of the most important events in human history, the causes of the French Revolution are complex and are still debated among historians. Following the Seven Years War and the American Revolutionary War, the French government was deeply in debt, Years of bad harvests leading up to the Revolution also inflamed popular resentment of the privileges enjoyed by the clergy and the aristocracy. Demands for change were formulated in terms of Enlightenment ideals and contributed to the convocation of the Estates-General in May 1789, a central event of the first stage, in August 1789, was the abolition of feudalism and the old rules and privileges left over from the Ancien Régime. The next few years featured political struggles between various liberal assemblies and right-wing supporters of the intent on thwarting major reforms. The Republic was proclaimed in September 1792 after the French victory at Valmy, in a momentous event that led to international condemnation, Louis XVI was executed in January 1793. External threats closely shaped the course of the Revolution, internally, popular agitation radicalised the Revolution significantly, culminating in the rise of Maximilien Robespierre and the Jacobins. Large numbers of civilians were executed by revolutionary tribunals during the Terror, after the Thermidorian Reaction, an executive council known as the Directory assumed control of the French state in 1795. The rule of the Directory was characterised by suspended elections, debt repudiations, financial instability, persecutions against the Catholic clergy, dogged by charges of corruption, the Directory collapsed in a coup led by Napoleon Bonaparte in 1799. The modern era has unfolded in the shadow of the French Revolution, almost all future revolutionary movements looked back to the Revolution as their predecessor. The values and institutions of the Revolution dominate French politics to this day, the French Revolution differed from other revolutions in being not merely national, for it aimed at benefiting all humanity. Globally, the Revolution accelerated the rise of republics and democracies and it became the focal point for the development of all modern political ideologies, leading to the spread of liberalism, radicalism, nationalism, socialism, feminism, and secularism, among many others. The Revolution also witnessed the birth of total war by organising the resources of France, historians have pointed to many events and factors within the Ancien Régime that led to the Revolution. Over the course of the 18th century, there emerged what the philosopher Jürgen Habermas called the idea of the sphere in France. A perfect example would be the Palace of Versailles which was meant to overwhelm the senses of the visitor and convince one of the greatness of the French state and Louis XIV. Starting in the early 18th century saw the appearance of the sphere which was critical in that both sides were active. In France, the emergence of the public sphere outside of the control of the saw the shift from Versailles to Paris as the cultural capital of France. In the 1750s, during the querelle des bouffons over the question of the quality of Italian vs, in 1782, Louis-Sébastien Mercier wrote, The word court no longer inspires awe amongst us as in the time of Louis XIV
16.
Champagne (province)
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Champagne is a historical province in the northeast of France, now best known as the Champagne wine region for the sparkling white wine that bears its name. It was founded in 1065 near the city of Provins and was made up of different counties descended from the medieval kingdom of Austrasia. Formerly ruled by the counts of Champagne, its edge is about 100 miles east of Paris. The cities of Troyes, Reims, and Épernay are the centers of the area. Most of Champagne is now part of the French administrative region of Champagne-Ardenne, which comprises four departments, Ardennes, Aube, Haute-Marne, and Marne. The name Champagne comes from the Latin campania and referred to the similarities between the hills of the province and the Italian countryside of Campania located south of Rome. In the High Middle Ages, the province was famous for the Champagne Fairs which were important in the economy of the Western societies. The chivalric romance had its first beginnings in the county of Champagne with the famous writer Chrétien de Troyes who wrote stories of the Round Table from the Arthurian legends, a few counts of Champagne were French kings and some of them were even Kings of France and of Navarre. Counts of Champagne were highly considered by the French aristocracy
17.
French Army
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The French Army, officially the Land Army is the land-based and largest component of the French Armed Forces. Along with the French Air Force, the French Navy and the National Gendarmerie, the current Chief of Staff of the French Army is General Jean-Pierre Bosser, a direct subordinate of the Chief of the Defence Staff. All soldiers are considered professionals following the suspension of conscription, voted in parliament in 1997, as of 2014, the French Army employed 111,628 personnel. In addition, the element of the French Army consisted of 15,453 personnel of the Operational Reserve. The Kings of France needed reliable troops during and after the Hundred Years War and these units of troops were raised by issuing ordonnances to govern their length of service, composition and payment. These Compagnies dordonnance formed the core of the Gendarme Cavalry into the sixteenth century, stationed throughout France and summoned into larger armies as needed. There was also made for Francs-archers units of bowmen and foot soldiers raised from the non-noble classes. The bulk of the infantry for warfare was still provided by urban or provincial militias, raised from an area or city to fight locally and named for their recruiting grounds. Gradually these units became more permanent, and in 1480s Swiss instructors were recruited and these men would be paid and contracted and receive training. Henry II further regularised the French army by forming standing Infantry regiments to replace the Militia structure, the first of these the Régiments de Picardie, Piémont, Navarre and Champagne were called the Les Vieux Corps. It was normal policy to disband regiments after a war was over as a cost saving measure with the Vieux Corps and the Kings own Household Troops the Maison du Roi being the only survivors. Regiments could be raised directly by the King and so called after the region in which they were raised, or by the nobility and so called after the noble or his appointed colonel. In 1684 there was a reorganisation of the French infantry and again in 1701 to fit in with Louis XIVs plans. This reshuffle created many of the regiments of the French Army and standardised their equipment. The army of the Sun King tended to wear coats with coloured linings. There were exceptions and the troops, recruited from outside France. In addition to these regiments of the line the Maison du Roi provided several elite units, the Swiss Guards, French Guards, the revolution split the army with the main mass losing most of its officers to aristocratic flight or guillotine and becoming demoralised and ineffective. The French Guard joined the revolt and the Swiss Guards were massacred during the storming of the Tuileries palace, under Napoleon I, the French Army conquered most of Europe during the Napoleonic Wars
18.
Salisbury Plain
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Salisbury Plain is a chalk plateau in central southern England covering 300 square miles. It is part of a system of chalk downlands throughout eastern and southern England formed by the rocks of the Chalk Group and largely lies within the county of Wiltshire, the plain is famous for its rich archaeology, including Stonehenge, one of Englands best known landmarks. Additionally the plain has arable land, and a few areas of beech trees. Its highest point is Easton Hill, the boundaries of Salisbury Plain have never been truly defined, and there is some difference of opinion as to its exact area. The river valleys surrounding it, and other downs and plains beyond them loosely define its boundaries, to the north the scarp of the downs overlooks the Vale of Pewsey, and to the north west the Bristol Avon. The River Wylye runs along the south west, and the Bourne runs to the east, the Hampshire Avon runs through the eastern half of the plain and to the south the plain peters out as the river valleys close together before meeting at Salisbury. From here the Avon continues south to the English Channel at Christchurch, the Hampshire Downs and the Berkshire Downs are chalk downland to the east and north of Salisbury Plain, and the Dorset Downs is to the south west. In the west and north west the geology is mainly of the clays and limestones of the Blackmore Vale, the A303 road runs along the southern area of the plain, while the A345 and the A360 cut across the centre. Salisbury Plain is famous for its history and archaeology, in the Neolithic period Stone Age man began to settle on the plain, most likely centred around the causewayed enclosure of Robin Hoods Ball. Large long barrows like White Barrow and other earthworks were built across the plain, by 2500 BC areas around Durrington Walls and Stonehenge had become a focus for building, and the southern part of the plain continued to be settled into the Bronze Age. Roman roads are visible features, probably serving a settlement near Old Sarum, villas are sparse, however, and Anglo-Saxon place names suggest that the plain was mostly a grain-producing imperial estate. In the 6th century Anglo-Saxon incomers built planned settlements in the valleys surrounded by strip lynchets, the cathedral is evidence of the prosperity the wool and cloth trade brought to the area. In the mid-19th century the wool and cloth industry began to decline, leading to a decline in the population and change in use from sheep farming to agriculture. Wiltshire became one of the poorest counties in England during this period of decline, there are a number of chalk carvings on the plain, of which the most famous is the Westbury White Horse. The Kennet and Avon Canal was constructed to the north of the plain, in 1896, George Kemp and Guglielmo Marconi experimented with wireless telegraphy on Salisbury Plain, and achieved good results over a distance of 1.75 miles. Media related to Army Training Estate Salisbury Plain at Wikimedia Commons The military training area covers roughly half of the plain, the army first conducted exercises on the plain in 1898. From that time, the Ministry of Defence bought up large areas of land until the Second World War, the MoD now own 150 square miles of land, making it the largest military training area in the United Kingdom. Of this, around 39 square miles are permanently closed to the public, as of 2016, the largest camps and barracks are at Larkhill, Bulford, Tidworth, Trenchard Lines and Warminster
19.
Ardennes (department)
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Ardennes is a department in the Grand Est region of northeastern France named after the Ardennes area. Its prefecture is the town Charleville-Mézières, the inhabitants of the department are known as Ardennais or Ardennaises. The department is surrounded by the French departments of Aisne to the west, Marne to the south, Meuse to the east and by the Belgian province of Namur to the north. It is traversed in its part by the winding valley of the Meuse and it is in this part of the department that the majority of people. Charleville-Mézières and Sedan are the urban centres. The department is part of the Academy of Reims and under the jurisdiction of the Court of Appeal of Reims, the INSEE and Post Code is 08. With an area of 5,229 square kilometres, the Ardennes was the smallest of the four departments that made up the region Champagne-Ardenne and it nevertheless presents a degree of geographical diversity. The highest point of the department is 504m and is situated on the slopes of the Croix Scaille. It is in part of the Ardennes mountains that the Meuse winds through a picturesque valley. Flowing into the part of the Ardennes department it waters both upstream and downstream the main cities of Sedan, Charleville-Mézières, and Nouzonville. It has numerous tributaries – the main ones in the department being the Semois, the Ardennes department does not have a uniform climate throughout its territory especially not during the winter period. All this stems from the location of the department, which is midway between the English Channel, the North Sea and the interior of Europe and this difference can be easily observed in practice. This nuance of climate is also evident by the difference with the adjoining regions. Despite a high rate, the department continues to lose population,300,000 in 2000 due to high unemployment. The two world wars have each time resulted in a loss of population, there were 330,000 people at the end of the 19th century. The communes, however, are gaining inhabitants and this highly contemporary concept favours commuting between Home and Work. This is the phenomenon of suburbanization which has become common in the whole of France from which Ardennes does not escape, on 1 January 2006, the Ardennes population stood at 295,653 inhabitants. The population is declining in urban areas but five times less than in rural areas, the limited decline in the urban space where two thirds of the Ardennes people live is the result of two opposite dynamics
20.
Meuse (department)
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Meuse is a department in northeast France, named after the River Meuse. Parts of Meuse belong to Parc naturel régional de Lorraine, front lines in trench warfare during World War I ran varying courses through the department and it hosted an important battle/offensive in 1916 in and around Verdun. Meuse is one of the original 83 departments created during the French Revolution on 4 March 1790, the new departments were to be uniformly administered and approximately equal to one another in size and population. The department was created from the provinces of Barrois and Three Bishoprics. From about 500 AD, the Franks controlled this part of northeastern France, the Carolingian territories were divided into three sections in 843 at the Treaty of Verdun, and the area that is now the department of Meuse, became part of Middle Francia. Lothair II died without heirs and Lotharingia was divided into an east and west part. The Battle of Sedan was fought in the part of the department during the Franco-Prussian War in 1870. It resulted in the capture of the Emperor Napoleon III and large numbers of his troops and effectively decided the war in favour of Prussia, the area was again a battleground in World War I when the Battle of Verdun was fought in 1916. In the Second World War it again saw action in battle when the Germans sought to establish a base from which to capture the Meuse bridges. Meuse is a department in northeastern France and is part of the region of Grand Est, the capital and largest town in the department is Bar-le-Duc, and other large towns are Commercy and Verdun. The main rivers flowing through the department are the River Meuse, the Aire, a ridge running from south to north separates the watersheds of the Seine and the Rhine. These hills are called the Argonne and are clothed in oak forests, the area of the department is 2,408 sq mi. The principal crops grown are wheat, barley and oats, potatoes, oilseed rape, vegetables, livestock is raised and timber is extracted from the forests. The main industries are brewing and the manufacture of glass and tiles, lace-making is a traditional craft in the department. Part of the department is in the Lorraine Regional Natural Park, the park has many natural habitats including calcareous grassland, forested valleys, wet meadows, ponds and streams. There are many Natura 2000 protected areas and it is an important resting area for migratory birds, among the different habitats it includes a stretch of coast, the plain of Woëvre, the Lac de Madine, the Meuse valley and the Hague plateau. The total area of the park is 205,000 hectares, since the mid-nineteenth century, the exodus of the countryside inhabitants to the cities has caused the population of rural France to fall. Meuse has no big cities to receive population and the population of the department has thus decreased
21.
Haute-Marne
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Haute-Marne is a department in the northeast of France named after the Marne River. Haute-Marne is one of the original 83 departments created during the French Revolution on March 4,1790 and it was created from parts of the former provinces of Champagne, Burgundy, Lorraine and Franche-Comté. In March 1814 the departmental prefecture, Chaumont, was the witness to the end of the First Empire. On 1 March, Prussia, Russia, the United Kingdom and Austria signed an accord forbidding any individual peace deal with Napoleon I, during World War II, Haute-Marne was partitioned under German occupation. The canal which runs from the Marne to the Saône served as a border, the east was a reserved zone, intended for the creation of a new German state, whereas to the west would be the traditional occupied zone. Haute-Marne was finally liberated by the Allies, in the form of the division of General Leclerc, Haute-Marne is part of the region of Grand Est and is surrounded by the departments of Meuse, Vosges, Haute-Saône, Côte-dOr, Aube, and Marne. The nearest big cities are Paris, Nancy, Strasbourg, Basel, the highest mountain is Haut-du-Sac, in the Langres Plateau, in the southwest of the department, which rises to a height of 516 m. The lowest points at 117m are found on the plains of Perthois, the department is named after the Marne River, whose source is near Langres. This river covers 120 kilometres within the department, the department is to the east of the Parisian basin, and is characterised by a concentric sequence of cliff faces of varying geological origin, oriented northeast/southwest. The Haute-Marne department is not a department but this peaceful territory has numerous interesting places to present. Indeed, the department was one of the most powerful in French history thanks to metallurgy economy and was a land of confrontations along history, thus, among other examples, the French Wars of Religion began with the Massacre of Vassy in the north of the Haute-Marne department. Following this event, open military conflicts across France Kingdom began, the Edict of Nantes is the consequence of this period
22.
Aube
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Aube is a French department in the Grand Est region of north-eastern France. As with sixty departments in France, this department is named after a river, with 305,606 inhabitants, Aube is 76th department in terms of population. The inhabitants of the department are known as Aubois or Auboises The department was constituted as it is today by a decree of the National Assembly of 15 January 1790, the Aube department is located in the south-west side of the Grand Est region. It borders the departments of Marne in the north, Haute-Marne to the east, Côte-dOr in the south-east, Yonne in the south-west, major cities with more than 10,000 inhabitants) are, Troyes, Romilly-sur-Seine, La Chapelle-Saint-Luc, Saint-André-les-Vergers and Sainte-Savine. They are mostly located in the centre of the department, four of those five cities are part of the Agglomeration of Troyes. There are 23 rivers throughout the department, the four main rivers being the Seine, the Aube, the Armance, the department has 140,000 hectares of forests. Located in the Community of communes of Forests, lakes, and lands in Champagne, in the same place, there is the Orient Lake and the Amance and Temple lakes where fishing, recreational water sports, and bathing are available. Each lake specialises in one or more of these activities, the climate is moderate without intense cold or excessive heat which represents a climate similar to continental and oceanic. Between 1950 and 1985 the average temperature recorded in the department was 10.1 °C which is equivalent to the Paris basin. The average sunshine hours per year is 1771, average annual rainfall is quite high. In general there is rain in autumn than in winter. In contrast summer is the season when rainfall is lowest, there is, however, more rain in the south-east than the north-west. Prevailing wind is from the west, the department has 150 km of autoroutes,33 km of national roads,4,517 km of departmental roads and 2,116 km of local roads. In the Agglomeration of Troyes TCAT provides a network between communes. Unlike many networks that are provided by operators, the agglomeration community of the city is the owner of the company. The network currently serves eleven communes including two outside the Troyes agglomeration, other cities, including Romilly-sur-Seine, have no transport network. Aube also has intercity transport networks,21 regular bus routes are operated between the major cities of the department. The use of lines is entrusted to private coaches, Transdev - The Carriers of Aube has 15 routes, Keolis Sud Lorraine has 4 routes, Procars Champagne has 2 routes
23.
Seine-et-Marne
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Seine-et-Marne is a French department, named after the Seine and Marne rivers, and located in the Île-de-France region. Seine-et-Marne is one of the original 83 departments, created on 4 March 1790 and it had previously belonged to the former province of Île-de-France. With 60% of the used as farmland, Seine-et-Marne is where most agricultural activity occurs within the Île-de-France. Cereals and sugar beet are the exports from Seine-et-Marne. The other key structures are the refinery at Grandpuits and the Snecma research plant. The two new towns are the centre of tourism for the department, mainly due to parks such as Disneyland Park. Seine-et-Marne has a temperate Atlantic climate, the average rainfall is based upon that of Fontainebleau, giving an average rainfall of 650 mm, which is higher than the average of Île-de-France. Average temperature in Melun during the 1953–2002 period was 3.2 °C for January and 18.6 °C for July, the storm of 26 December 1999 led to five deaths in Seine-et-Marne and caused several trees to fall. Seine-et-Marne forms a part of the region, the department covers 49% of the regions land area. It is bordered by Val-dOise, Seine-Saint-Denis, Val-de-Marne, Essonne to the West, Loiret and Yonne to the South, Aube and Marne to the East, the department has many natural reserves, notably Brie and Gâtinais. The highest point of the département is Saint-Georges Hill, people from Seine-et-Marne are known as the Seine-et-Marnais. Originally Seine-et-Marne was very rural and lightly populated, over the past 50 years, however, its population has tripled, due to the development of the Paris conurbation and the building of new towns in the northwest of the region. The population was estimated to be 1,267,496 inhabitants in 2006, the region has changed from consisting only of small villages to forming a large part of the Paris conurbation. Seine-et-Marne as a whole shares a sister city relationship with Orlando, Florida, United States, mutualité, assurance et cycles de lincendie
24.
Aisne
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Aisne is a French department in the Hauts-de-France region of northern France. It is named after the river Aisne, the department of Aisne is surrounded by the French departments of Nord, Somme, Oise, Ardennes, and Seine-et-Marne and borders Belgium to the northeast. The Aisne River crosses the area from east to west, where it joins the Oise River, the Marne forms part of the southern boundary of the department with the department of Seine-et-Marne. The southern part of the department is the region known as la Brie poilleuse. According to the 2003 census, the area of the department was 123,392 hectares. The landscape is dominated by masses of rock which often have steep flanks and these rocks appear all over the region, but the most impressive examples are at Laon and the Chemin des Dames ridge. The principal cities in Aisne are, Laon, pop,15,000 Condren Chauny Hirson Villers-Cotterêts La Fère Vervins Guise See also, List of the communes of the Aisne department and Brie. The Scheldt, the Aisne, the Marne, the Ourcq, the Vesle, the Somme, the Oise, in the south of the department, there is the Surmelin, the Verdonnelle, and the Dhuys. The department is crossed by numerous canals. In 1873, the department of Aisne had 10 railway companies with a length of 382 km. There is an average of 500 to 750 mm precipitation annually, weather Data for Saint Quentin - Roupy Aisne is one of the original 83 departments created during the French Revolution on 4 March 1790. It was created from parts of the provinces of Île-de-France, Picardy. Most of the old growth forests in the area were destroyed during battles in World War I, the French offensive against the Chemin des Dames in spring 1917 is sometimes referred to as the Second Battle of the Aisne. Agriculture dominates the economy, especially cereal crops, beet sugar is one of the most important industrial crops of the area. Silk, cotton, and wool weaving flourish in Saint-Quentin and other towns, saint-Gobain is known for its production of mirrors, which started in the 17th century. Guise is the centre of the northern area of Aisne. The department is a mixture of rural areas and working-class towns, the smaller cities of the northern department such as Guise, Hirson, Vervins and the railway city of Tergnier are sources of support for left-wing parties. The President of the General Council is the Socialist Yves Daudigny, Aisne is divided into five arrondissements and 21 cantons
25.
Chalk
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Chalk is a soft, white, porous, sedimentary carbonate rock, a form of limestone composed of the mineral calcite. Calcite is a salt called calcium carbonate or CaCO3. It forms under reasonably deep marine conditions from the accumulation of minute calcite shells shed from micro-organisms called coccolithophores. Flint is very common as bands parallel to the bedding or as embedded in chalk. It is probably derived from sponge spicules or other organisms as water is expelled upwards during compaction. Flint is often deposited around larger fossils such as Echinoidea which may be silicified, Chalk as seen in Cretaceous deposits of Western Europe is unusual among sedimentary limestones in the thickness of the beds. Most cliffs of chalk have very few obvious bedding planes unlike most thick sequences of such as the Carboniferous Limestone or the Jurassic oolitic limestones. This presumably indicates very stable conditions over tens of millions of years, Chalk has greater resistance to weathering and slumping than the clays with which it is usually associated, thus forming tall steep cliffs where chalk ridges meet the sea. Chalk hills, known as chalk downland, usually form where bands of chalk reach the surface at an angle, because chalk is well jointed it can hold a large volume of ground water, providing a natural reservoir that releases water slowly through dry seasons. Chalk is mined from chalk deposits both above ground and underground, Chalk mining boomed during the Industrial Revolution, due to the need for chalk products such as quicklime and bricks. Abandoned chalk mines remain a popular tourist attraction due to their massive expanse, the Chalk Group is a European stratigraphic unit deposited during the late Cretaceous Period. It forms the famous White Cliffs of Dover in Kent, England, the Champagne region of France is mostly underlain by chalk deposits, which contain artificial caves used for wine storage. Some of the highest chalk cliffs in the occur at Jasmund National Park in Germany. Ninety million years ago what is now the chalk downland of Northern Europe was ooze accumulating at the bottom of a great sea. Chalk was one of the earliest rocks made up of particles to be studied under the electron microscope. Their shells were made of calcite extracted from the rich sea-water, as they died, a substantial layer gradually built up over millions of years and, through the weight of overlying sediments, eventually became consolidated into rock. Later earth movements related to the formation of the Alps raised these former sea-floor deposits above sea level, the chemical composition of chalk is calcium carbonate, with minor amounts of silt and clay. It is formed in the sea by plankton, which fall to the sea floor and are then consolidated and compressed during diagenesis into chalk rock
26.
Eocene
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The Eocene Epoch, lasting from 56 to 33.9 million years ago, is a major division of the geologic timescale and the second epoch of the Paleogene Period in the Cenozoic Era. The Eocene spans the time from the end of the Paleocene Epoch to the beginning of the Oligocene Epoch. The start of the Eocene is marked by a period in which the concentration of the carbon isotope 13C in the atmosphere was exceptionally low in comparison with the more common isotope 12C. As with other periods, the strata that define the start and end of the epoch are well identified. The name Eocene comes from the Ancient Greek ἠώς and καινός, the Eocene epoch is conventionally divided into early, middle, and late subdivisions. The corresponding rocks are referred to as lower, middle, the Ypresian stage constitutes the lower, the Priabonian stage the upper, and the Lutetian and Bartonian stages are united as the middle Eocene. The Eocene Epoch contained a variety of different climate conditions that includes the warmest climate in the Cenozoic Era. During this period of time, little to no ice was present on Earth with a difference in temperature from the equator to the poles. Following the maximum was a descent into an icehouse climate from the Eocene Optimum to the Eocene-Oligocene transition at 34 million years ago. During this decrease ice began to reappear at the poles, greenhouse gases, in particular carbon dioxide and methane, played a significant role during the Eocene in controlling the surface temperature. For the early Eocene there is discussion on how much carbon dioxide was in the atmosphere. This is due to numerous proxies representing different atmospheric carbon dioxide content, for contrast, today the carbon dioxide levels are at 400 ppm or 0. 04%. At about the beginning of the Eocene Epoch the amount of oxygen in the atmosphere more or less doubled. During the early Eocene, methane was another gas that had a drastic effect on the climate. In comparison to carbon dioxide, methane has much effect on temperature as methane is ~34 times more effective per molecule than carbon dioxide on a 100-year scale. Most of the methane released to the atmosphere during this period of time would have been from wetlands, swamps, the atmospheric methane concentration today is 0. 000179% or 1.79 ppmv. Due to the climate and sea level rise associated with the early Eocene, more wetlands, more forests. Comparing the early Eocene production of methane to current levels of atmospheric methane, biogenic production of methane produces carbon dioxide and water vapor along with the methane, as well as yielding infrared radiation
27.
Oligocene
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The Oligocene is a geologic epoch of the Paleogene Period and extends from about 33.9 million to 23 million years before the present. As with other geologic periods, the rock beds that define the epoch are well identified but the exact dates of the start. The name Oligocene comes from the Ancient Greek ὀλίγος and καινός, the Oligocene is preceded by the Eocene Epoch and is followed by the Miocene Epoch. The Oligocene is the third and final epoch of the Paleogene Period, the Oligocene is often considered an important time of transition, a link between the archaic world of the tropical Eocene and the more modern ecosystems of the Miocene. Major changes during the Oligocene included an expansion of grasslands. By contrast, the Oligocene–Miocene boundary is not set at an easily identified worldwide event, Oligocene faunal stages from youngest to oldest are, The Paleogene Period general temperature decline is interrupted by an Oligocene 7-million-year stepwise climate change. A deeper 8.2 °C,400, 000-year temperature depression leads the 2 °C, the stepwise climate change began 32.5 Ma and lasted through to 25.5 Ma, as depicted in the PaleoTemps chart. The Oligocene climate change was a increase in ice volume. The 7-million-year depression abruptly terminated within 1–2 million years of the La Garita Caldera eruption at 28–26 Ma, a deep 400, 000-year glaciated Oligocene Miocene boundary event is recorded at McMurdo Sound and King George Island. During this epoch, the continued to drift toward their present positions. Antarctica became more isolated and finally developed an ice cap, a brief marine incursion marks the early Oligocene in Europe. Marine fossils from the Oligocene are rare in North America, there appears to have been a land bridge in the early Oligocene between North America and Europe, since the faunas of the two regions are very similar. Sometime during the Oligocene, South America was finally detached from Antarctica and it also allowed the Antarctic Circumpolar Current to flow, rapidly cooling the Antarctic continent. Angiosperms continued their expansion throughout the world as tropical and sub-tropical forests were replaced by deciduous forests. Open plains and deserts became more common and grasses expanded from their habitat in the Eocene moving out into open tracts. However, even at the end of the period, grass was not quite enough for modern savannas. In North America, subtropical species dominated with cashews and lychee trees present, and temperate trees such as roses, beeches, the legumes spread, while sedges, bulrushes, and ferns continued their ascent. Even more open landscapes allowed animals to grow to larger sizes than they had earlier in the Paleocene epoch 30 million years earlier, marine faunas became fairly modern, as did terrestrial vertebrate fauna on the northern continents
28.
Vesle
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The Vesle is the river on which the city of Reims stands. It is a fourth order river of France and a tributary of the Aisne. It is 140 kilometres long, rises in the département of Marne through which it flows most of its course, though still passing through the chalk country, it soon begins to flow on its own Holocene deposits. On leaving the western outskirts, it enters the much more wooded landscape of the Eocene geology. The info box photograph shows the Vesle as it passes through fen carr, halfway From Reims to Soissons, at Fismes the river receives the river Ardre from its left bank. At Condé-sur-Aisne, having descended to an altitude of about 45 metres, from Sept Saulx, some 20 km. above Reims, and into the city, the river is paralleled by the Aisne to Marne Canal. Below Reims, its valley accommodates the road, now the N31/E46, the Noblette joins from the right bank near Vadenay, the Cheneu joins from the right bank at Mourmelon-le-Petit, the Fosse joins from the left bank at Muizon. The Ardre is its principal tributary and it joins from the left bank, at Fismes. The Vesle is a river of medium flow, like most which come from the chalkland of the Champagne-Ardenne région and its flow was recorded over a period of 34 years, at Braine, in the department of Aisne. That is to say a short of its confluence with the Aisne. The catchment area down to point is 1,440 km². The yearly mean flow or discharge of the river at Braine is 7.72 m3/s, seasonal fluctuations in the flow are very small. The N31 road has seen the passage of many kings, emperors, the French kings were crowned at Reims and usually returned to Paris this way. The rivers upper reaches pass over the plain of Champaigne Once rather disparagingly called Champaigne Pouilleuse, because of its poverty. This region has long used for military training, its geology. The training ground nearest to it is at the Camp de Mourmelon, during the Great War of 1914-18, the rivers valley was just behind the French-held front but at times, particularly in the spring and summer of 1918, it was heavily fought over. See Second Battle of the Marne, two important natural zones of ecological, zoological and botanical interest, have been decreed on the length of the Vesle. The first is upstream from Reims and designated as The great fens of the Vesle Valley from Prunay to Courmelois
29.
Aube (river)
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The Aube is a river in France, right tributary of the Seine. The river gives its name to the Aube département and its source is in the Haute-Marne département, on the plateau of Langres, near the town Auberive. It flows through the départements Haute-Marne, Côte-dOr, Aube, and it flows into the river Seine near Marcilly-sur-Seine. Cities along the river include Bar-sur-Aube and Arcis-sur-Aube. geoportail. fr The Aube at the Sandre database Media related to Aube River at Wikimedia Commons
30.
Seine
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The Seine is a 777-kilometre-long river and an important commercial waterway within the Paris Basin in the north of France. It rises at Source-Seine,30 kilometres northwest of Dijon in northeastern France in the Langres plateau, flowing through Paris and it is navigable by ocean-going vessels as far as Rouen,120 kilometres from the sea. There are 37 bridges within Paris and dozens more spanning the river outside the city, examples in Paris include the Pont Alexandre III and Pont Neuf, the latter of which dates back to 1607. Outside the city, examples include the Pont de Normandie, one of the longest cable-stayed bridges in the world, the Seine rises in the commune of Source-Seine, about 30 kilometres northwest of Dijon. The source has been owned by the city of Paris since 1864, a number of closely associated small ditches or depressions provide the source waters, with an artificial grotto laid out to highlight and contain a deemed main source. The grotto includes a statue of a nymph, on the same site are the buried remains of a Gallo-Roman temple. Small statues of the dea Sequana Seine goddess and other ex voti found at the place are now exhibited in the Dijon archeological museum. The Seine is dredged and oceangoing vessels can dock at Rouen,120 kilometres from the sea, commercial riverboats can use the river from Bar-sur-Seine,560 kilometres to its mouth. At Paris, there are 37 bridges, the river is only 24 metres above sea level 446 kilometres from its mouth, making it slow flowing and thus easily navigable. The Seine Maritime,105.7 kilometres from the English Channel at Le Havre to Rouen, is the portion of the Seine used by ocean-going craft. The tidal section of the Seine Maritime is followed by a section with four large multiple locks until the mouth of the Oise at Conflans-Sainte-Honorine. Multiple locks at Bougival / Chatou and at Suresnes lift the vessels to the level of the river in Paris, upstream from Paris seven locks ensure navigation to Saint Mammès, where the Loing mouth is situated. Through an eighth lock the river Yonne is reached at Montereau-Fault-Yonne, from the mouth of the Yonne, larger ships can continue upstream to Nogent-sur-Seine. From there on, the river is only by small craft. All navigation ends abruptly at Marcilly-sur-Seine, where the ancient Canal de la Haute-Seine used to allow vessels to continue all the way to Troyes and this canal has been abandoned for many years. The average depth of the Seine today at Paris is about 9.5 metres. Until locks were installed to raise the level in the 1800s, the river was much shallower within the city most of the time, today the depth is tightly controlled and the entire width of the river between the built-up banks on either side is normally filled with water. The average flow of the river is low, only a few cubic metres per second
31.
Kings of France
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The monarchs of the Kingdom of France and its predecessors ruled from the establishment of the Kingdom of the Franks in 486 till the fall of the Second French Empire in 1870. Sometimes included as kings of France are the kings of the Franks of the Merovingian dynasty, which ruled from 486 until 751, and of the Carolingians, who ruled until 987. The Capetian dynasty, the descendants of Hugh Capet, included the first rulers to adopt the title of king of France for the first time with Philip II. The Capetians ruled continuously from 987 to 1792 and again from 1814 to 1848, the branches of the dynasty which ruled after 1328, however, are generally given the specific branch names of Valois and Bourbon. During the brief period when the French Constitution of 1791 was in effect and after the July Revolution in 1830 and it was a constitutional innovation known as popular monarchy which linked the monarchs title to the French people rather than to the possession of the territory of France. With the House of Bonaparte Emperors of the French ruled in 19th century France and it was used on coins up to the eighteenth century. During the brief period when the French Constitution of 1791 was in effect and after the July Revolution in 1830 and it was a constitutional innovation known as popular monarchy which linked the monarchs title to the French people rather than to the possession of the territory of France. They used the title Emperor of the French and this article lists all rulers to have held the title King of the Franks, King of France, King of the French or Emperor of the French. For other Frankish monarchs, see List of Frankish kings, in addition to the monarchs listed below, the Kings of England and Great Britain from 1340–60, 1369-1420, and 1422–1801 also claimed the title of King of France. For a short time, this had some basis in fact – under the terms of the 1420 Treaty of Troyes, Charles VI had recognized his son-in-law Henry V of England as regent and heir. Henry V predeceased Charles VI and so Henry Vs son, Henry VI, most of Northern France was under English control until 1435, but by 1453, the English had been expelled from all of France save Calais, and Calais itself fell in 1558. Nevertheless, English and then British monarchs continued to claim the title for themselves until the creation of the United Kingdom in 1801. The Merovingians were a Salian Frankish dynasty that ruled the Franks for nearly 300 years in a known as Francia in Latin. Their territory largely corresponded to ancient Gaul as well as the Roman provinces of Raetia, Germania Superior, the Carolingian dynasty was a Frankish noble family with origins in the Arnulfing and Pippinid clans of the 7th century AD. In 751, a Carolingian, Pepin the Younger, dethroned the Merovingians and with the consent of the Papacy, the Robertians were Frankish noblemen owing fealty to the Carolingians, and ancestors of the subsequent Capetian dynasty. Odo, Count of Paris, was chosen by the western Franks to be their king following the removal of emperor Charles the Fat, the Bosonids were a noble family descended from Boso the Elder, their member, Rudolph, was elected King of the Franks in 923. After the death of Louis V, the son of Hugh the Great and grandson of Robert I, the Capetian Dynasty, the male-line descendants of Hugh Capet, ruled France continuously from 987 to 1792 and again from 1814 to 1848. They were direct descendants of the Robertian kings, the cadet branches of the dynasty which ruled after 1328, however, are generally given the specific branch names of Valois and Bourbon
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Coronation of the French monarch
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The accession of the King of France was legitimized by coronation ceremony performed with the Crown of Charlemagne at Notre-Dame de Reims. The most important part of the French coronation ceremony was not the coronation itself, the Carolingian king Pepin the Short was the first anointed monarch in Europe, which occurred in Soissons to legitimize the accession of the new dynasty. A second coronation of Pepin by Pope Stephen II took place at the Basilica of St Denis in 754, the first coronation performed by a Pope. Since this Roman glass vial containing the balm due to be mixed with chrism, was brought by the dove of the Holy Spirit. All succeeding Kings of France were anointed with this same oil—mixed with chrism prior to their coronation, French queens were crowned either together with their husband at Rheims or alone at Sainte-Chapelle or Abbey of St. Denis. The king is crowned by the Archbishop of Reims who is assisted by four bishops of his ecclesiastical province. The established order of six bishops is, The Archbishop of Reims anoints, the Bishop of Laon carries the holy ampulla. The Bishop of Langres carries the scepter, the Bishop of Beauvais carries and shows the coat of arms or royal mantle. The Bishop of Chalons carries the royal ring, the Bishop of Noyon carries the belt. To these are added the Abbot of the Abbey of Saint-Remi, guardian of the ampulla. Peers are cited for the first time in 1203 and 1226, however, their first recorded participation in the coronation is made on the occasion of the coronation of Philip V of France on 9 January 1317. These are the six aforementioned ecclesiastical peers and the six lay peers, in order of protocol, the six lay peers are, The Duke of Burgundy carries the royal crown, girds the kings sword, and gives him the order of chivalry. The Duke of Normandy carries the first square banner, the Duke of Aquitaine carries the second square banner. The Count of Toulouse carries the spurs, the Count of Flanders carries the royal sword. The Count of Champagne carries the banner of war, the spiritual peerages were perpetual, and were never extinguished during the existence of the Kingdom of France. But as early as 1204, the roster of the lay peerages had been incomplete, Normandy had been absorbed into the French crown, Toulouse in 1271, Champagne in 1284. Aquitaine was several times forfeited and restored, Burgundy became extinct in 1361 and again in 1477, hence, more often than not, princes of the royal blood and high-ranking members of the nobility acted as representatives of the ancient lay peerages. Spiritual peers were also represented if their see is vacant or they are unable to attend
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Lake Der-Chantecoq
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Lake Der-Chantecoq is situated close to the commune of Saint-Dizier in the departments of Marne and Haute-Marne. It is the largest artificial lake in Western Europe, covering 48 km2 with 350 million m³ of water, the lake is named after the Der plain, in which it is located, and the submerged village Chantecoq. The lake is fed by a 12 km long canal that branches off the river Marne in Saint-Dizier, the outflow of the lake is a canal that joins the Marne in Arrigny,20 km downstream of Saint-Dizier. The lake is located in the communes Sainte-Marie-du-Lac-Nuisement, Éclaron-Braucourt-Sainte-Livière, Giffaumont-Champaubert, Arrigny, Larzicourt and it was created in 1974 to hold the water of the River Marne so that flooding of the Seine at Paris would stop. It is managed by Les Grands Lacs de Seine and its construction required the destruction of three villages, Chantecoq, Champaubert-aux-Bois and Nuisement-aux-Bois. Today, many sports are popular here, including sailing, water skiing, jet-ski. The combination of water, islands, and freshwater marshes make the area ideal for waterfowl. Each spring and autumn, tens of thousands of cranes assemble here in their migration between wintering grounds to the south and breeding sites in northern Europe, other birds recorded in the area include white-tailed eagle, great egret, and various geese, ducks, loons, and grebes. The surrounding area is rural, a region of farmland and forest, lac du Der en Champagne Yaughting Club du Der Club Nautique
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