Pierre François Bosquet
Pierre François Joseph Bosquet was a French Army general. He served during the conquest of the Crimean War. Bosquet was born in Landes. Here he soon made himself remarkable not only for technical skill but the moral qualities indispensable for high command. Becoming captain in 1839, he distinguished himself at the actions of Sidi-Lakhdar and Oued-Melah, he was soon given the command of a battalion of native tirailleurs, in 1843 was thanked in general orders for his brilliant work against the Flittahs. In 1845 he became lieutenant-colonel, in 1847 colonel of a French line regiment. In the following year he was in charge of the Oran district, where his swift suppression of an insurrection won him further promotion to the grade of general of brigade, in which rank he went through the campaign of Kabulia, receiving a severe wound. In 1853 he returned to France after a general of division. Bosquet was amongst the earliest chosen to serve in the Crimean War, at the Battle of Alma his division led the French attack.
When the Anglo-French troops formed the siege of Sevastopol, Bosquet's corps of two divisions protected them against interruption. Referring to the Charge of the Light Brigade, Bosquet muttered the memorable line: C’est magnifique, mais ce n’est pas la guerre: c'est de la folie, his timely intervention at the Battle of Inkerman secured the victory for the allies. During 1855 Bosquet's corps occupied the right wing of the besieging armies opposite the Mamelon and Malakov, he himself led his corps at the storming of the Mamelon, at the grand assault of 8 September he was in command of the whole of the storming troops. In the struggle for the Malakov he received another serious wound. At the age of forty-five Bosquet, now one of the foremost soldiers in Europe, became a senator and a Marshal of France, but he was in poor health, he lived only a few years longer, he was awarded the Knight Grand Cross of the Order of the Bath, the Grand Cross of the Légion d'honneur and the Order of the Medjidie 1st Class.
Légion d'honneur Knight Officer Commander Grand Officer Grand Cross Médaille militaire Honorary Knight Grand Cross of the Order of the Bath Crimea Medal
Communes of France
The commune is a level of administrative division in the French Republic. French communes are analogous to civil townships and incorporated municipalities in the United States and Canada, Gemeinden in Germany, comuni in Italy or ayuntamiento in Spain; 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 are vested with significant powers to manage the populations and land of the geographic area covered; the communes are the fourth-level administrative divisions of France. Communes vary in size and area, from large sprawling cities with millions of inhabitants like Paris, to small hamlets with only a handful of inhabitants. Communes 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, the difference residing in the lack of administrative powers.
Except for the municipal arrondissements of its largest cities, the communes are the lowest level of administrative division in France and are governed by elected officials with extensive autonomous powers to implement national policy. A commune is city, or other municipality. "Commune" in English has a historical bias, implies an association with socialist political movements or philosophies, collectivist lifestyles, or particular history. There is nothing intrinsically different between commune in French; the French word commune appeared in the 12th century, from Medieval Latin communia, for a large gathering of people sharing a common life. 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, because French communes still reflect the division of France into villages or parishes at the time of the French Revolution. The whole territory of the French Republic is divided into communes.
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, it was 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. COM of Saint Barthélemy, it was a commune inside the Guadeloupe region. The commune structure was abolished when Saint-Barthélemy became an overseas collectivity on 22 February 2007. Furthermore, two regions without permanent habitation have no communes: TOM of the French Southern and Antarctic Lands Clipperton Island in the Pacific Ocean In metropolitan France, the average area of a commune in 2004 was 14.88 square kilometres. The median area of metropolitan France's communes at the 1999 census was smaller, at 10.73 square kilometres. 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 median area of communes is 22 km2. Switzerland and the Länder of Rhineland-Palatinate, Schleswig-Holstein, Thuringia in Germany were the only places in Europe where the communes had a smaller median area than in France; the communes of France's overseas départements such as Réunion and French Guiana are large by French standards. They group into the same commune several villages or towns with sizeable distances among them. In Réunion, demographic expansion and sprawling urbanization have resulted in the administrative splitting of some communes; the median population of metropolitan France's communes at the 1999 census was 380 inhabitants. Again this is a small number, here France stands apart in Europe, with the lowest communes' median population of all the European countries; this small median population of French communes can be compared with Italy, where the median population of communes in 2001 was 2,343 inhabitants, Belgium, or Spain.
The median population given here should not hide the fact that there are pronounced differences in size between French communes. As mentioned in the introduction, a commune can be a city of 2 million inhabitants such as Paris, a town of 10,000 inhabitants, or just a hamlet of 10 inhabitants. What the median population tells us is that the vast majority of the French communes only have a few hundred inhabitants. In metropolitan France just over 50 percent of the 36,683 communes have fewer than 500 inhabitants a
Charles Despiau was a French sculptor. Charles-Albert Despiau was born at Mont-de-Marsan and attended first the École des Arts Décoratifs and the École nationale supérieure des Beaux-Arts, he began exhibiting at the Salon des Artistes Français, from 1898 to 1900. Rodin hired him as an assistant in 1907. Despiau worked with Rodin, as well as doing his own sculpture, until 1914, when he was drafted for service in the camouflage unit in World War I. Returning to sculpture after the war, his success was established with his one-man show at the Brummer Gallery in New York in late 1927, he died in Paris in 1946. Despiau was not a prolific sculptor, preferring to work for as long as it took to realize his vision. There are several surviving plaster statues, his works portraits and nudes exemplifying a calm classicism, are in the collections of over thirty museums in France and over 100 museums around the world, including the Metropolitan Museum of Art. The Museum of Modern Art in New York owns the bronze Assia his best-known work.
The largest collection is in his native Mont-de-Marsan, in a museum he shares with Robert Wlérick, established in the Donjon Lacataye. Despiau produced a total of 1,000 drawings over a fifty-year career. Despiau at www.ilovefiguresculpture.com Charles Despiau website Charles Despiau in American public collections, on the French Sculpture Census website
Sedimentary rocks are types of rock that are formed by the accumulation or deposition of small particules and subsequent cementation of mineral or organic particles on the floor of oceans or other bodies of water at the Earth's surface. Sedimentation is the collective name for processes; the particles that form a sedimentary rock are called sediment, may be composed of geological detritus or biological detritus. Before being deposited, the geological detritus was formed by weathering and erosion from the source area, transported to the place of deposition by water, ice, mass movement or glaciers, which are called agents of denudation. Biological detritus was formed by bodies and parts of dead aquatic organisms, as well as their fecal mass, suspended in water and piling up on the floor of water bodies. Sedimentation may occur as dissolved minerals precipitate from water solution; the sedimentary rock cover of the continents of the Earth's crust is extensive, but the total contribution of sedimentary rocks is estimated to be only 8% of the total volume of the crust.
Sedimentary rocks are only a thin veneer over a crust consisting of igneous and metamorphic rocks. Sedimentary rocks are deposited in layers as strata; the study of sedimentary rocks and rock strata provides information about the subsurface, useful for civil engineering, for example in the construction of roads, tunnels, canals or other structures. Sedimentary rocks are important sources of natural resources like coal, fossil fuels, drinking water or ores; the study of the sequence of sedimentary rock strata is the main source for an understanding of the Earth's history, including palaeogeography and the history of life. The scientific discipline that studies the properties and origin of sedimentary rocks is called sedimentology. Sedimentology is part of both geology and physical geography and overlaps with other disciplines in the Earth sciences, such as pedology, geomorphology and structural geology. Sedimentary rocks have been found on Mars. Sedimentary rocks can be subdivided into four groups based on the processes responsible for their formation: clastic sedimentary rocks, biochemical sedimentary rocks, chemical sedimentary rocks, a fourth category for "other" sedimentary rocks formed by impacts and other minor processes.
Clastic sedimentary rocks are composed of other rock fragments that were cemented by silicate minerals. Clastic rocks are composed of quartz, rock fragments, clay minerals, mica. Clastic sedimentary rocks, are subdivided according to the dominant particle size. Most geologists use the Udden-Wentworth grain size scale and divide unconsolidated sediment into three fractions: gravel and mud; the classification of clastic sedimentary rocks parallels this scheme. This tripartite subdivision is mirrored by the broad categories of rudites and lutites in older literature; the subdivision of these three broad categories is based on differences in clast shape, grain size or texture. Conglomerates are dominantly composed of rounded gravel, while breccias are composed of dominantly angular gravel. Sandstone classification schemes vary but most geologists have adopted the Dott scheme, which uses the relative abundance of quartz and lithic framework grains and the abundance of a muddy matrix between the larger grains.
Composition of framework grains The relative abundance of sand-sized framework grains determines the first word in a sandstone name. Naming depends on the dominance of the three most abundant components quartz, feldspar, or the lithic fragments that originated from other rocks. All other minerals are considered accessories and not used in the naming of the rock, regardless of abundance. Quartz sandstones have >90% quartz grains Feldspathic sandstones have <90% quartz grains and more feldspar grains than lithic grains Lithic sandstones have <90% quartz grains and more lithic grains than feldspar grainsAbundance of muddy matrix material between sand grains When sand-sized particles are deposited, the space between the grains either remains open or is filled with mud. "Clean" sandstones with open pore space are called arenites. Muddy sandstones with abundant muddy matrix are called wackes. Six sandstone names are possible using the descriptors for grain composition and the amount of matrix. For example, a quartz arenite would be composed of quartz grains and have little or no clayey matrix between the grains, a lithic wacke would have abundant lithic grains and abundant muddy matrix, etc.
Although the Dott classification scheme is used by sedimentologists, common names like greywacke and quartz sandstone are still used by non-specialists and in popular literature. Mudrocks are sedimentary rocks composed of at least 50% silt- and clay-sized particles; these fine-grained particles are transported by turbulent flow in water or air, deposited as the flow calms and the particles settle out of suspension. Most authors presently
Romanesque architecture is an architectural style of medieval Europe characterized by semi-circular arches. There is no consensus for the beginning date of the Romanesque style, with proposals ranging from the 6th to the 11th century, this date being the most held. In the 12th century it developed into the Gothic style, marked by pointed arches. Examples of Romanesque architecture can be found across the continent, making it the first pan-European architectural style since Imperial Roman architecture; the Romanesque style in England is traditionally referred to as Norman architecture. Combining features of ancient Roman and Byzantine buildings and other local traditions, Romanesque architecture is known by its massive quality, thick walls, round arches, sturdy pillars, barrel vaults, large towers and decorative arcading; each building has defined forms of regular, symmetrical plan. The style can be identified right across Europe, despite regional characteristics and different materials. Many castles were built during this period, but they are outnumbered by churches.
The most significant are the great abbey churches, many of which are still standing, more or less complete and in use. The enormous quantity of churches built in the Romanesque period was succeeded by the still busier period of Gothic architecture, which or rebuilt most Romanesque churches in prosperous areas like England and Portugal; the largest groups of Romanesque survivors are in areas that were less prosperous in subsequent periods, including parts of southern France, rural Spain and rural Italy. Survivals of unfortified Romanesque secular houses and palaces, the domestic quarters of monasteries are far rarer, but these used and adapted the features found in church buildings, on a domestic scale. According to the Oxford English Dictionary, the word "Romanesque" means "descended from Roman" and was first used in English to designate what are now called Romance languages; the French term "romane" was first used in the architectural sense by archaeologist Charles de Gerville in a letter of 18 December 1818 to Auguste Le Prévost to describe what Gerville sees as a debased Roman architecture.
In 1824 Gerville's friend Arcisse de Caumont adopted the label "roman" to describe the "degraded" European architecture from the 5th to the 13th centuries, in his Essai sur l'architecture religieuse du moyen-âge, particulièrement en Normandie, at a time when the actual dates of many of the buildings so described had not been ascertained: The name Roman we give to this architecture, which should be universal as it is the same everywhere with slight local differences has the merit of indicating its origin and is not new since it is used to describe the language of the same period. Romance language is degenerated Latin language. Romanesque architecture is debased Roman architecture; the first use in a published work is in William Gunn's An Inquiry into the Origin and Influence of Gothic Architecture. The word was used by Gunn to describe the style, identifiably Medieval and prefigured the Gothic, yet maintained the rounded Roman arch and thus appeared to be a continuation of the Roman tradition of building.
The term is now used for the more restricted period from the late 10th to 12th centuries. The term "Pre-romanesque" is sometimes applied to architecture in Germany of the Carolingian and Ottonian periods and Visigothic and Asturian constructions between the 8th and the 10th centuries in the Iberian Peninsula while "First Romanesque" is applied to buildings in north of Italy and Spain and parts of France that have Romanesque features but pre-date the influence of the Abbey of Cluny. Typical Romanesque architectural forms Buildings of every type were constructed in the Romanesque style, with evidence remaining of simple domestic buildings, elegant town houses, grand palaces, commercial premises, civic buildings, city walls, village churches, abbey churches, abbey complexes and large cathedrals. Of these types of buildings and commercial buildings are the most rare, with only a handful of survivors in the United Kingdom, several clusters in France, isolated buildings across Europe and by far the largest number unidentified and altered over the centuries, in Italy.
Many castles exist, the foundations of. Most have been altered, many are in ruins. By far the greatest number of surviving Romanesque buildings are churches; these range from tiny chapels to large cathedrals. Although many have been extended and altered in different styles, a large number remain either intact or sympathetically restored, demonstrating the form and decoration of Romanesque church architecture; the scope of Romanesque architecture Romanesque architecture was the first distinctive style to spread across Europe since the Roman Empire. With the decline of Rome, Roman building methods survived to an extent in Western Europe, where successive Merovingian and Ottonian architects continued to build large stone buildings such as monastery churches and palaces. In the more northern countries, Roman building styles and techniques had never been adopted except for official buildings, while in Scandinavia they were unknown. Although the round arch continued in use, the engineering skills required to vault large spaces and build large domes were lost.
There was a loss of stylistic continuity apparent in the decline of the formal vocabulary of the Classical Orders. In Rome several great Constantinian basilicas continued in use as an inspiration to builders; some traditions of Rom
The Midou or Midour is the left precursor of the Midouze, in the Southwest of France. The Midou rises in the Gers département, it joins the Douze in Mont-de-Marsan to constitute a tributary of the Adour. Gers: by Nogaro Landes: Villeneuve-de-Marsan, Mont-de-Marsan Riberette or Midour de Devant. Midouzon, from Termes-d'Armagnac, Estang. Ludon, from Le Houga. N. B.: = right tributary.
The Landes is a department in southwestern France. Landes is one of the original 83 departments that were created during the French Revolution on 4 March 1790, it was created from parts of the provinces of Gascony. During the first part of the nineteenth century large parts of the department were covered with poorly drained heathland, the origin of its name; the vegetation covered rich soil and was periodically burned off, leaving excellent pasturage for sheep, which around 1850 are thought to have numbered between 900,000 and 1,000,000 in this area. The sheep were managed by shepherds who moved around on stilts and became proficient at covering long distances thus supported. Most of the sheep departed during the second half of the nineteenth century when systematic development of large pine plantations transformed the landscape and the local economy. One of the most famous citizens of the Landes was the nineteenth-century French economist Frederic Bastiat; the Nobel Prize–winning novelist François Mauriac set his novels in the Landes.
The Landes is part of the current region of Nouvelle-Aquitaine and is surrounded by the departments of Gironde, Lot-et-Garonne and Pyrénées-Atlantiques, as well as the Atlantic Ocean on the west. With an area stretching over more than 9000 km², Landes is, after Gironde, the second largest department of the metropolitan French territory, it is well known for the Côte d'Argent beach, Europe's longest, attracts many surfers to Mimizan and Hossegor each year. It is home to a château called Château de Gaujacq, built in 1686; the President of the General Council is Xavier Fortinon. In terms of agriculture, the Landes is known for its large pine forest, the raw material for a timber and resin industries in the region; the forest was planted in the early nineteenth century to prevent erosion of the region's sandy soil by the sea. Cantons of the Landes department Communes of the Landes department Arrondissements of the Landes department Prefecture website Conseil Général website Landes at Curlie