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Accous
Accous is a commune in the Pyrénées-Atlantiques department in the Nouvelle-Aquitaine region in southwestern France. Geography Location Accous is located some 30 km south of Oloron-Sainte-Marie in the Aspe Valley, one of the three valleys of the High-Béarn, the other valleys being the Ossau Valley in the east and Barétous valley in the west. From the Spanish border on its southern edge, it stretches along Le Labadie river to the point where it joins the Gave d'Aspe. From this river junction, the Gave d'Aspe forms the western border of the rest of the commune which extends a further 10 kilometres to the east with the Lac du Montagnon at the northeastern edge. Access The commune is accessed from the north by the E7 motorway. This highway follows the western border of the commune along the Gave d'Aspe then crosses the narrow neck of the commune before continuing to the Spanish border near Candanchu. To access Accous village it is necessary to follow one of a number o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Accous (Pyr-Atl, Fr) Pont D'Esquir, Cascade Descendant Du Bois D'Arapoup
Accous is a commune in the Pyrénées-Atlantiques department in the Nouvelle-Aquitaine region in southwestern France. Geography Location Accous is located some 30 km south of Oloron-Sainte-Marie in the Aspe Valley, one of the three valleys of the High-Béarn, the other valleys being the Ossau Valley in the east and Barétous valley in the west. From the Spanish border on its southern edge, it stretches along Le Labadie river to the point where it joins the Gave d'Aspe. From this river junction, the Gave d'Aspe forms the western border of the rest of the commune which extends a further 10 kilometres to the east with the Lac du Montagnon at the northeastern edge. Access The commune is accessed from the north by the E7 motorway. This highway follows the western border of the commune along the Gave d'Aspe then crosses the narrow neck of the commune before continuing to the Spanish border near Candanchu. To access Accous village it is necessary to follow one of a number o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Accous (Pyr-Atl, Fr) Ruisseau La Berthe
Accous is a commune in the Pyrénées-Atlantiques department in the Nouvelle-Aquitaine region in southwestern France. Geography Location Accous is located some 30 km south of Oloron-Sainte-Marie in the Aspe Valley, one of the three valleys of the High-Béarn, the other valleys being the Ossau Valley in the east and Barétous valley in the west. From the Spanish border on its southern edge, it stretches along Le Labadie river to the point where it joins the Gave d'Aspe. From this river junction, the Gave d'Aspe forms the western border of the rest of the commune which extends a further 10 kilometres to the east with the Lac du Montagnon at the northeastern edge. Access The commune is accessed from the north by the E7 motorway. This highway follows the western border of the commune along the Gave d'Aspe then crosses the narrow neck of the commune before continuing to the Spanish border near Candanchu. To access Accous village it is necessary to follow one of a number o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gave D'Aspe
The Gave d'Aspe is a torrential river flowing through the Aspe Valley, one of the three main valleys of the High-Béarn (Pyrénées-Atlantiques), in the southwest of France. It is long. It is formed in the ''Aspe Cirque'', below the Aspe peak, elevation , in Spain. After joining the Gave d'Ossau, in Oloron-Sainte-Marie, it forms the Gave d'Oloron. Main tributaries * (R) ''Arnousse'' * (L) ''Gave de Baralet'' * (R) ''Sescouet'' * (L) ''Gave de Bélonce'' * (R) ''Escuarpe'', in Cette-Eygun * (L) ''Gave de Lescun'' * (R) ''Berthe'', from Accous * (L) ''Malugar'', from Athas * (L) ''Arricq d'Osse'' * (R) ''Gabarret'', aka ''Gave d'Aydius'' * (R) ''Barrescou'', from the Marie-Blanque Pass * (L) '' Lourdios'' * (R) ''Ourtau'' Départements and towns * Pyrénées-Atlantiques Pyrénées-Atlantiques (; Gascon Occitan: ''Pirenèus Atlantics''; eu, Pirinio Atlantiarrak or ) is a department in the southwest corner of France and of the region of Nouvelle-Aquitaine. Named after the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Aspe Valley
The Aspe Valley is a valley in the French part of the Pyrenees, department of Pyrénées-Atlantiques. Geography It is one of the three valleys located in the historic region of upper Béarn, along with the Ossau Valley to the east and Barétous Valley to the west. The valley of Aspe stretches for 25 miles along the river Gave d'Aspe, roughly going from the town of Escot to the Spanish border where it meets the Aragon Valley, named after the Spanish river. Thirteen towns, or communes, are established in the valley. From the north to the south, these are: Escot, Lourdios-Ichère, Sarrance, Bedous, Osse-en-Aspe, Aydius, Accous, Lées-Athas, Lescun, Cette-Eygun, Etsaut, Borce and Urdos. Language The traditional dialect spoken in the valley is Gascon, a regional variety of Occitan language. History The region has been invaded by many groups through its history: Moors, Romans, Germanic tribes, as well as kingdoms in Spain. In 1620, the sovereign state of Béarn, in which the v ... [...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] |
Volcanic
A volcano is a rupture in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface. On Earth, volcanoes are most often found where tectonic plates are diverging or converging, and most are found underwater. For example, a mid-ocean ridge, such as the Mid-Atlantic Ridge, has volcanoes caused by divergent tectonic plates whereas the Pacific Ring of Fire has volcanoes caused by convergent tectonic plates. Volcanoes can also form where there is stretching and thinning of the crust's plates, such as in the East African Rift and the Wells Gray-Clearwater volcanic field and Rio Grande rift in North America. Volcanism away from plate boundaries has been postulated to arise from upwelling diapirs from the core–mantle boundary, deep in the Earth. This results in hotspot volcanism, of which the Hawaiian hotspot is an example. Volcanoes are usually not created where two tectonic plate ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Triassic
The Triassic ( ) is a geologic period and system which spans 50.6 million years from the end of the Permian Period 251.902 million years ago ( Mya), to the beginning of the Jurassic Period 201.36 Mya. The Triassic is the first and shortest period of the Mesozoic Era. Both the start and end of the period are marked by major extinction events. The Triassic Period is subdivided into three epochs: Early Triassic, Middle Triassic and Late Triassic. The Triassic began in the wake of the Permian–Triassic extinction event, which left the Earth's biosphere impoverished; it was well into the middle of the Triassic before life recovered its former diversity. Three categories of organisms can be distinguished in the Triassic record: survivors from the extinction event, new groups that flourished briefly, and other new groups that went on to dominate the Mesozoic Era. Reptiles, especially archosaurs, were the chief terrestrial vertebrates during this time. A specialized subgroup of archo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dolerites
Diabase (), also called dolerite () or microgabbro, is a mafic, holocrystalline, subvolcanic rock equivalent to volcanic basalt or plutonic gabbro. Diabase dikes and sills are typically shallow intrusive bodies and often exhibit fine-grained to aphanitic chilled margins which may contain tachylite (dark mafic glass). ''Diabase'' is the preferred name in North America, while ''dolerite'' is the preferred name in the rest of the English-speaking world, where sometimes the name ''diabase'' refers to altered dolerites and basalts. Some geologists prefer to avoid confusion by using the name ''microgabbro''. The name ''diabase'' comes from the French ', and ultimately from the Greek - meaning "act of crossing over, transition". Petrography Diabase normally has a fine but visible texture of euhedral lath-shaped plagioclase crystals (62%) set in a finer matrix of clinopyroxene, typically augite (20–29%), with minor olivine (3% up to 12% in olivine diabase), magnetite (2%), and i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glacier
A glacier (; ) is a persistent body of dense ice that is constantly moving under its own weight. A glacier forms where the accumulation of snow exceeds its Ablation#Glaciology, ablation over many years, often Century, centuries. It acquires distinguishing features, such as Crevasse, crevasses and Serac, seracs, as it slowly flows and deforms under stresses induced by its weight. As it moves, it abrades rock and debris from its substrate to create landforms such as cirques, moraines, or fjords. Although a glacier may flow into a body of water, it forms only on land and is distinct from the much thinner sea ice and lake ice that form on the surface of bodies of water. On Earth, 99% of glacial ice is contained within vast ice sheets (also known as "continental glaciers") in the polar regions, but glaciers may be found in mountain ranges on every continent other than the Australian mainland, including Oceania's high-latitude oceanic island countries such as New Zealand. Between lati ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Institut Géographique National
An institute is an organisational body created for a certain purpose. They are often research organisations (research institutes) created to do research on specific topics, or can also be a professional body. In some countries, institutes can be part of a university or other institutions of higher education, either as a group of departments or an autonomous educational institution without a traditional university status such as a "university institute" (see Institute of Technology). In some countries, such as South Korea and India, private schools are sometimes referred to as institutes, and in Spain, secondary schools are referred to as institutes. Historically, in some countries institutes were educational units imparting vocational training and often incorporating libraries, also known as mechanics' institutes. The word "institute" comes from a Latin word ''institutum'' meaning "facility" or "habit"; from ''instituere'' meaning "build", "create", "raise" or "educate". ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gave (placename Element)
The French word ''gave'' is a generic name referring to torrential rivers, in the west side of the Pyrenees. In the central part of the Pyrenees, the name ''neste'' has the same function. The word ''gave'' derives from the old Gascon ''gabar'', attested as ''gabarrus'' in medieval Latin.Theodule (8th century - 9th century) Based on a pre-Celtic root ''*gab'' meaning 'hollow' (thus 'throat'), it refers to lower places, valleys and rivers. It is widely found in placenames of Gascony as Gabardan, Gavarret, Gavarnie, Gabas, etc. The name of the ''Gabali'' (the ancient people living in Gévaudan) is supposed to be related to this stem. The final ''-r'' is missing because it was lost in Gascon: gabar > gabà > . Gaves in the Pyrenees * gaves réunis * gave d'Arrens * gave d'Aspe, * gave d' Aspé, * gave de Baralet, * gave de Bélonce, * gave de Bious, * gave de Brousset, * gave de Cauterets, * gave de Cestrède, * gave d' Estaubé, * gave du Lavedan, * gave de Gaube, * gave d ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bedous
Bedous is a commune of the Pyrénées-Atlantiques department in southwestern France. It is the birthplace of Pierre Laclède, the Frenchman who founded the U.S. city of St. Louis. Its station on the Pau–Canfranc railway was closed after an accident in 1970, but re-opened in 2016 as the terminus of service from Pau. See also *Communes of the Pyrénées-Atlantiques department The following is a list of the 546 communes of the Pyrénées-Atlantiques department of France. The communes cooperate in the following intercommunalities (as of 2020):Communes of Pyrénées-Atlantiques [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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