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Aureille
Aureille (; oc, Aurelha) is a commune in the Bouches-du-Rhône department in the Provence-Alpes-Côte d'Azur region of southern France. The inhabitants of the commune are known as ''Aureillois'' or ''Aureilloises'' in French. The commune has been awarded one flower by the ''National Council of Towns and Villages in Bloom'' in the ''Competition of cities and villages in Bloom''. Geography Location Aureille is located between the Alpilles mountain chain and the Crau plain some 8 km from Eyguières in the east and 8 km from Mouriès in the west. It is dominated by the ''Signal of Opiès'', the highest point in the commune, in the north-east. It is a member of the communes of the Baux Valley but traditionally it is closer to the city of Arles. Access Road D17 passes through the commune south of the town from Eyguières in the east to Mouries in the west. Road D25A branches off this road in the commune and goes to the village then continues north to join the D25 just ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Paul Révoil
Amédée Marie Joseph Paul Révoil (3 May 1856 – 28 April 1914) was a French diplomat and administrator who represented France in Morocco (1896–1901), was Governor General of Algeria (1901–1903) and was French ambassador to Switzerland (1906) and Spain (1907–09). He is known for his role in moving towards a peaceful extension of French influence in Morocco. Early years (1856–95) Amédée Marie Joseph Paul Révoil was born on 3 May 1856 in Nîmes, Gard. His parents were Henri Antoine Révoil (1822–1900), Chief Architect in the Monuments Historiques, and Louise Henriette Anaïs Baragnon (1829–1870). He studied law and published his thesis for a license, ''De l'Usufruit'', in Paris on 30 May 1877. He was a member of the Conférence Molé-Tocqueville, where on 13 March 1877 his proposal to limit the Legion of Honour decoration to military services was examined. Paul Révoil was Chief of Staff of Jules Develle at the Ministry of Agriculture from 1890 to 1893 before fo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alpilles
The Chaîne des Alpilles is a small range of low mountains in Provence, southern France, located about south of Avignon. Geography The range is an extension of the much larger Luberon range. Although it is not high - some 498 m (1,634 ft) at its highest point - the Alpilles range stands out impressively, as it rises abruptly from the Rhône valley and from the very flat alluvial plain of Crau. The range is about 25 km long by about 8 to 10 km wide, running in an east-west direction between the Rhône and Durance rivers. The landscape of the Alpilles is one of arid limestone peaks separated by dry valleys. Communes The Chaîne des Alpilles is part of the territory of 15 communes: Aureille, Les Baux-de-Provence, Eygalières, Eyguières, Fontvieille, Mas-Blanc-des-Alpilles, Maussane-les-Alpilles, Mouriès, Paradou, Orgon, Saint-Étienne-du-Grès, Saint-Martin-de-Crau, Saint-Rémy-de-Provence, Sénas, Tarascon. Flora and fauna The lower slopes are planted wit ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mouriès
Mouriès (; oc, Moriés, ) is a commune in the Bouches-du-Rhône department in southern France. Population Economy Mouriès is known for its olive oil production, calling itself "the olive oil capital of France" (a claim disputed by Nyons, further north). There are still two working olive oil mills in town, including one which allows tours. In December of every year there is a festival celebrating the end of the harvest and the new oil, with a small parade and the benediction of the oil, along with various markets. Wednesday is market day. The small tourism office in town supplies a list of all of the market days in the area. In winter the market here is much larger than in the other towns in the area ( Maussane, Aureille or Eygalières). File:140604-Mouries-Markt-03.jpg, market in Mouriès, Cours Paul Revoil File:140604-Mouries-Markt-01.jpg, market in Mouriès, Cours Paul Revoil File:140604-Mouries-Markt-02.jpg, market in Mouriès, Cours Paul Revoil File:140604-Mouries ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Communes Of France
The () is a level of administrative division in the French Republic. French are analogous to civil townships and incorporated municipalities in the United States and Canada, ' in Germany, ' in Italy, or ' in Spain. The United Kingdom's equivalent are civil parishes, although some areas, particularly urban areas, are unparished. are based on historical geographic communities or villages and are vested with significant powers to manage the populations and land of the geographic area covered. The are the fourth-level administrative divisions of France. vary widely in size and area, from large sprawling cities with millions of inhabitants like Paris, to small hamlets with only a handful of inhabitants. typically are based on pre-existing villages and facilitate local governance. All have names, but not all named geographic areas or groups of people residing together are ( or ), the difference residing in the lack of administrative powers. Except for the municipal arrondi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Marseille
Marseille ( , , ; also spelled in English as Marseilles; oc, Marselha ) is the prefecture of the French department of Bouches-du-Rhône and capital of the Provence-Alpes-Côte d'Azur region. Situated in the camargue region of southern France, it is located on the coast of the Gulf of Lion, part of the Mediterranean Sea, near the mouth of the Rhône river. Its inhabitants are called ''Marseillais''. Marseille is the second most populous city in France, with 870,731 inhabitants in 2019 (Jan. census) over a municipal territory of . Together with its suburbs and exurbs, the Marseille metropolitan area, which extends over , had a population of 1,873,270 at the Jan. 2019 census, the third most populated in France after those of Paris and Lyon. The cities of Marseille, Aix-en-Provence, and 90 suburban municipalities have formed since 2016 the Aix-Marseille-Provence Metropolis, an Indirect election, indirectly elected Métropole, metropolitan authority now in charge of wider metropo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mediterranean Climate
A Mediterranean climate (also called a dry summer temperate climate ''Cs'') is a temperate climate sub-type, generally characterized by warm, dry summers and mild, fairly wet winters; these weather conditions are typically experienced in the majority of Mediterranean-climate regions and countries, but remain highly dependent on proximity to the ocean, altitude and geographical location. This climate type's name is in reference to the coastal regions of the Mediterranean Sea within the Mediterranean Basin, where this climate type is most prevalent. The "original" Mediterranean zone is a massive area, its western region beginning with the Iberian Peninsula in southwestern Europe and coastal regions of northern Morocco, extending eastwards across southern Europe, the Balkans, and coastal Northern Africa, before reaching a dead-end at the Levant region's coastline. Mediterranean climate zones are typically located along the western coasts of landmasses, between roughly 30 and 45 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Canal Craponne Aureille By Malost
Canals or artificial waterways are waterways or engineered channels built for drainage management (e.g. flood control and irrigation) or for conveyancing water transport vehicles (e.g. water taxi). They carry free, calm surface flow under atmospheric pressure, and can be thought of as artificial rivers. In most cases, a canal has a series of dams and locks that create reservoirs of low speed current flow. These reservoirs are referred to as ''slack water levels'', often just called ''levels''. A canal can be called a ''navigation canal'' when it parallels a natural river and shares part of the latter's discharges and drainage basin, and leverages its resources by building dams and locks to increase and lengthen its stretches of slack water levels while staying in its valley. A canal can cut across a drainage divide atop a ridge, generally requiring an external water source above the highest elevation. The best-known example of such a canal is the Panama Canal. Many cana ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Étang De Berre
The Étang de Berre (in Provençal Occitan: ''estanh de Bèrra / mar de Bèrra'' according to classical orthography, ''estang de Berro / mar de Berro'' according to Mistralian orthography) is a brackish water lagoon on the Mediterranean coast of France, about north-west of Marseille. Geography The lagoon covers an area of . Created by the rise in water levels at the end of the Last Glacial Period (colloquially known as the last ice age), this small inland sea is composed of three parts: the principal body of water, the ''Étang de Vaïne'' to the east and the ''Étang de Bolmon'' to the south-east. The Étang de Berre is fed with fresh water by the rivers Arc, Touloubre and Cadière and – since 1966 – by Électricité de France's . Two canals link it to the Mediterranean, the open air leading towards Port-de-Bouc and the Canal de Marseille au Rhône which leads towards L'Estaque through the Rove Tunnel; the Rove Tunnel has been closed since 1963, after a section ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Early Cretaceous
The Early Cretaceous ( geochronological name) or the Lower Cretaceous (chronostratigraphic name), is the earlier or lower of the two major divisions of the Cretaceous. It is usually considered to stretch from 145 Ma to 100.5 Ma. Geology Proposals for the exact age of the Barremian-Aptian boundary ranged from 126 to 117 Ma until recently (as of 2019), but based on drillholes in Svalbard the defining early Aptian Oceanic Anoxic Event 1a (OAE1a) was carbon isotope dated to 123.1±0.3 Ma, limiting the possible range for the boundary to c. 122–121 Ma. There is a possible link between this anoxic event and a series of Early Cretaceous large igneous provinces (LIP). The Ontong Java-Manihiki-Hikurangi large igneous province, emplaced in the South Pacific at c. 120 Ma, is by far the largest LIP in Earth's history. The Ontong Java Plateau today covers an area of 1,860,000 km2. In the Indian Ocean another LIP began to form at c. 120 Ma, the Kerguelen P ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cretaceous
The Cretaceous ( ) is a geological period that lasted from about 145 to 66 million years ago (Mya). It is the third and final period of the Mesozoic Era, as well as the longest. At around 79 million years, it is the longest geological period of the entire Phanerozoic. The name is derived from the Latin ''creta'', "chalk", which is abundant in the latter half of the period. It is usually abbreviated K, for its German translation ''Kreide''. The Cretaceous was a period with a relatively warm climate, resulting in high eustatic sea levels that created numerous shallow inland seas. These oceans and seas were populated with now- extinct marine reptiles, ammonites, and rudists, while dinosaurs continued to dominate on land. The world was ice free, and forests extended to the poles. During this time, new groups of mammals and birds appeared. During the Early Cretaceous, flowering plants appeared and began to rapidly diversify, becoming the dominant group of plants across the Earth b ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jurassic
The Jurassic ( ) is a Geological period, geologic period and System (stratigraphy), stratigraphic system that spanned from the end of the Triassic Period million years ago (Mya) to the beginning of the Cretaceous Period, approximately Mya. The Jurassic constitutes the middle period of the Mesozoic, Mesozoic Era and is named after the Jura Mountains, where limestone strata from the period were first identified. The start of the Jurassic was marked by the major Triassic–Jurassic extinction event, associated with the eruption of the Central Atlantic magmatic province, Central Atlantic Magmatic Province. The beginning of the Toarcian Stage started around 183 million years ago and is marked by an extinction event associated with widespread Anoxic event, oceanic anoxia, ocean acidification, and elevated temperatures likely caused by the eruption of the Karoo-Ferrar, Karoo-Ferrar large igneous provinces. The end of the Jurassic, however, has no clear boundary with the Cretaceous and i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Molasse
__NOTOC__ The term "molasse" () refers to sandstones, shales and conglomerates that form as terrestrial or shallow marine deposits in front of rising mountain chains. The molasse deposits accumulate in a foreland basin, especially on top of flysch-like deposits, for example, those that left from the rising Alps, or erosion in the Himalaya. These deposits are typically the non-marine alluvial and fluvial sediments of lowlands, as compared to deep-water flysch sediments. Sedimentation stops when the orogeny stops, or when the mountains have eroded flat. Stanley, Steven M., ''Earth System History'', New York: W.H. Freeman and Company, 1999, p.243 The molasse can sometimes completely fill a foreland basin, creating a nearly flat depositional surface, that nonetheless remains a structural syncline. Molasse can be very thick near the mountain front, but usually thins out towards the interior of a craton; such massive, convex accumulations of sediment are known as ''clastic wedge I ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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