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Landepéreuse
Landepéreuse () is a former commune in the Eure department, in Normandy in northern France. On 1 January 2016, it was merged into the new commune of Mesnil-en-Ouche. Etymology The name "Landepereuse" derives from the Norman pronunciation of ''lande pierreuse'' ("stony ground"). The word ''lande'' comes from the Gaulish language, and refers to dry ground where few plants grow. "Stony" refers to the local abundance and size of stones. Geography Landepéreuse is a small rural village in the Pays d'Ouche, located in the south-western Eure. Its surface is 892 hectares. Its maximum altitude change is 48 m but ranges between 187 m in the south-west and 139 m in the north-east; the town hall is at 170 m. This slightly undulating countryside is characteristic of the topography in the Pays d'Ouche, already hinted at in the hills of the Perche country to the south and the Pays d'Auge a few kilometres to the west. The landscape is made up of fields, pastures, orchards and woods. These ar ...
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Mesnil-en-Ouche
Mesnil-en-Ouche (, literally '' Mesnil in Ouche'') is a commune in the department of Eure, northern France. The municipality was established on 1 January 2016 by merger of the 16 former communes of Ajou, La Barre-en-Ouche, Beaumesnil (the seat), Bosc-Renoult-en-Ouche, Épinay, Gisay-la-Coudre, Gouttiéres, Granchain, Jonquerets-de-Livet, Landepéreuse, La Roussière, Saint-Aubin-des-Hayes, Saint-Aubin-le-Guichard, Sainte-Marguerite-en-Ouche, Saint-Pierre-du-Mesnil Saint-Pierre-du-Mesnil () is a former commune in the Eure department in Normandy in northern France. On 1 January 2016, it was merged into the new commune of Mesnil-en-Ouche.Thevray.Ar ...
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Institut National De La Statistique Et Des études économiques
The National Institute of Statistics and Economic Studies (french: link=no, Institut national de la statistique et des études économiques), abbreviated INSEE or Insee ( , ), is the national statistics bureau of France. It collects and publishes information about the French economy and people and carries out the periodic national census. Headquartered in Montrouge, a commune in the southern Parisian suburbs, it is the French branch of Eurostat. The INSEE was created in 1946 as a successor to the Vichy regime's National Statistics Service (SNS). It works in close cooperation with the Institut national d'études démographiques (INED). Purpose The INSEE is responsible for the production and analysis of official statistics in France. Its best known responsibilities include: * Organising and publishing the national census. * Producing various indices – which are widely recognised as being of excellent quality – including an inflation index used for determining the rates o ...
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Holocene
The Holocene ( ) is the current geological epoch. It began approximately 11,650 cal years Before Present (), after the Last Glacial Period, which concluded with the Holocene glacial retreat. The Holocene and the preceding Pleistocene together form the Quaternary period. The Holocene has been identified with the current warm period, known as MIS 1. It is considered by some to be an interglacial period within the Pleistocene Epoch, called the Flandrian interglacial.Oxford University Press – Why Geography Matters: More Than Ever (book) – "Holocene Humanity" section https://books.google.com/books?id=7P0_sWIcBNsC The Holocene corresponds with the rapid proliferation, growth and impacts of the human species worldwide, including all of its written history, technological revolutions, development of major civilizations, and overall significant transition towards urban living in the present. The human impact on modern-era Earth and its ecosystems may be considered of global si ...
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Fontainebleau
Fontainebleau (; ) is a commune in the metropolitan area of Paris, France. It is located south-southeast of the centre of Paris. Fontainebleau is a sub-prefecture of the Seine-et-Marne department, and it is the seat of the ''arrondissement'' of Fontainebleau. The commune has the largest land area in the Île-de-France region; it is the only one to cover a larger area than Paris itself. The commune is closest to Seine-et-Marne Prefecture, Melun. Fontainebleau, together with the neighbouring commune of Avon and three other smaller communes, form an urban area of 36,724 inhabitants (2018). This urban area is a satellite of Paris. Fontainebleau is renowned for the large and scenic forest of Fontainebleau, a favourite weekend getaway for Parisians, as well as for the historic Château de Fontainebleau, which once belonged to the kings of France. It is also the home of INSEAD, one of the world's most elite business schools. Inhabitants of Fontainebleau are sometimes called '' ...
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Oligocene
The Oligocene ( ) is a geologic epoch of the Paleogene Period and extends from about 33.9 million to 23 million years before the present ( to ). As with other older geologic periods, the rock beds that define the epoch are well identified but the exact dates of the start and end of the epoch are slightly uncertain. The name Oligocene was coined in 1854 by the German paleontologist Heinrich Ernst Beyrich from his studies of marine beds in Belgium and Germany. The name comes from the Ancient Greek (''olígos'', "few") and (''kainós'', "new"), and refers to the sparsity of extant forms of molluscs. 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 a global expansion o ...
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Le Bosc-Renoult
Le Bosc-Renoult is a commune in the Orne department in northwestern France. Population See also *Communes of the Orne department The following is a list of the 385 communes of the Orne department of France. The communes cooperate in the following intercommunalities (as of 2020):Communes of Orne {{Orne-geo-stub ...
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Le Tréport
Le Tréport () is a commune in the Seine-Maritime department in Normandy, France. Geography A small fishing port and light industrial town situated in the Pays de Caux, some northeast of Dieppe at the junction of the D 940, the D 78 and the D 1015 roads. The mouth of the river Bresle meets the English Channel here, in between the high () chalk cliffs and the pebbly beach. Le Tréport-Mers station has rail connections to Beauvais. Le Tréport is also a sea-side resort and home to a casino. History Le Tréport (the ancient ''Ulterior Portus'') was a port of some note in the Middle Ages and suffered from the English invasions. Louis Philippe I twice received Queen Victoria here in 1843 and 1845. The casino was built 1896–1897. The British World War I soldier Arthur Bullock, who was stationed in Le Tréport after the Armistice, was captivated by the town, nestling at the bottom of cliffs which could be ascended by 365 steps or by a cliff railway. Bullock recorded in his ...
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Dieppe
Dieppe (; Norman: ''Dgieppe'') is a coastal commune in the Seine-Maritime department in the Normandy region of northern France. Dieppe is a seaport on the English Channel at the mouth of the river Arques. A regular ferry service runs to Newhaven in England. Famous for its scallops, Dieppe also has a popular pebbled beach, a 15th-century castle and the churches of Saint-Jacques and Saint-Remi. The mouth of the river Scie lies at Hautot-sur-Mer, directly to the west of Dieppe. The inhabitants of the town of Dieppe are called ''Dieppois'' (m) and ''Dieppoise'' (f) in French. History First recorded as a small fishing settlement in 1030, Dieppe was an important prize fought over during the Hundred Years' War. Dieppe housed the most advanced French school of cartography in the 16th century. Two of France's best navigators, Michel le Vasseur and his brother Thomas le Vasseur, lived in Dieppe when they were recruited to join the expedition of René Goulaine de Laudonnière whic ...
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Paleocene
The Paleocene, ( ) or Palaeocene, is a geological epoch (geology), epoch that lasted from about 66 to 56 mya (unit), million years ago (mya). It is the first epoch of the Paleogene Period (geology), Period in the modern Cenozoic Era (geology), Era. The name is a combination of the Ancient Greek ''palaiós'' meaning "old" and the Eocene Epoch (which succeeds the Paleocene), translating to "the old part of the Eocene". The epoch is bracketed by two major events in Earth's history. The K–Pg extinction event, brought on by Chicxulub impact, an asteroid impact and possibly volcanism, marked the beginning of the Paleocene and killed off 75% of living species, most famously the non-avian dinosaurs. The end of the epoch was marked by the Paleocene–Eocene Thermal Maximum (PETM), which was a major climatic event wherein about 2,500–4,500 gigatons of carbon were released into the atmosphere and ocean systems, causing a spike in global temperatures and ocean acidification. In the Pal ...
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Cenozoic
The Cenozoic ( ; ) is Earth's current geological era, representing the last 66million years of Earth's history. It is characterised by the dominance of mammals, birds and flowering plants, a cooling and drying climate, and the current configuration of continents. It is the latest of three geological eras since complex life evolved, preceded by the Mesozoic and Paleozoic. It started with the Cretaceous–Paleogene extinction event, when many species, including the non-avian dinosaurs, became extinct in an event attributed by most experts to the impact of a large asteroid or other celestial body, the Chicxulub impactor. The Cenozoic is also known as the Age of Mammals because the terrestrial animals that dominated both hemispheres were mammalsthe eutherians (placentals) in the northern hemisphere and the metatherians (marsupials, now mainly restricted to Australia) in the southern hemisphere. The extinction of many groups allowed mammals and birds to greatly diversify so that l ...
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Sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar (both silicates) because they are the most resistant minerals to weathering processes at the Earth's surface. Like uncemented sand, sandstone may be any color due to impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Since sandstone beds often form highly visible cliffs and other topographic features, certain colors of sandstone have been strongly identified with certain regions. Rock formations that are primarily composed of sandstone usually allow the percolation of water and other fluids and are porous enough to store large quantities, making them valuable aquifers and petroleum reservoirs. Quartz-bearing sandstone can be changed into quartzite through metamorphism, usually related to ...
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