Corbières Massif
The Corbières Massif (Catalan: ''Corberes''; french: Massif des Corbières, ) is a mountain range in the Pre-Pyrenees. It is the only true foothill of the Pyrenees on their northern side. Geography The Corbières are a mountain region in the Languedoc-Roussillon in southeastern France, located in the departements of Aude and Pyrénées-Orientales. The river Aude borders the Corbières to the west and north, and the river Agly more or less to the south. The eastern border is the Mediterranean Sea The Mediterranean Sea is a sea connected to the Atlantic Ocean, surrounded by the Mediterranean Basin and almost completely enclosed by land: on the north by Western and Southern Europe and Anatolia, on the south by North Africa, and on the .... The eastern part of the Corbières bordering the Mediterranean and the Etangs is also known as the ''Corbières Maritimes'', and has a special kind of climate and typical vegetation (thermo- mediterranean vegetation) which cannot be ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Puig De Bugarag
The Pic de Bugarach () or Pech de Bugarach () (''puèg de Bugarag'' in Occitan, i.e. "Peak of Bugarag") is the highest summit (1230 m) in the Corbières Massif in the French ''Midi''. The western part of the mountain is located on the territory of the commune of Bugarach. Its eastern part is on the territory of Camps-sur-l'Agly. The geology of the Pic de Bugarach is striking. Its top layer is an overthrust from the Iberian plate and is older than the bottom ones. This has given rise to its description as an "upside-down mountain". It is possible to climb up the Bugarach: a classical route called "Voie de la fenêtre" because of a big hole in a cliff, climbs the South face. One may go down via the easiest route, North, and join the "Col de Linas". Climbing still requires a good physical condition, and the mountain has claimed the life of at least one unprepared tourist. Esoterics Due to the mountain's unusual geology, a number of New Agers (called "esoterics" by local res ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Foothill
Foothills or piedmont are geographically defined as gradual increases in elevation at the base of a mountain range, higher hill range or an upland area. They are a transition zone between plains and low relief hills and the adjacent topographically higher mountains, hills, and uplands. Frequently foothills consist of alluvial fans, coalesced alluvial fans, and dissected plateaus. Description Foothills primarily border mountains, especially those which are reached through low ridges that increase in size closer and closer to the mountain, but can also border uplands and higher hills. Examples Areas where foothills exist, or areas commonly referred to as the foothills, include the: * Sierra Nevada foothills of California, USA * Foothills of the San Gabriel Valley in Los Angeles County, California, USA *Rocky Mountain Foothills in British Columbia and Alberta, Canada *Silesian Foothills in Silesia, Poland *Sivalik Hills along the Himalayas in the Indian subcontinent * Catalina ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Landforms Of Aude
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, Stratum, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountain A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Geology Of The Pyrenees
The Pyrenees are a 430-kilometre-long, roughly east–west striking, intracontinental mountain chain that divide France, Spain, and Andorra. The belt has an extended, polycyclic geological evolution dating back to the Precambrian. The chain's present configuration is due to the collision between the microcontinent Iberia and the southwestern promontory of the European Plate (i.e. Southern France). The two continents were approaching each other since the onset of the Upper Cretaceous (Albian/ Cenomanian) about 100 million years ago and were consequently colliding during the Paleogene (Eocene/Oligocene) 55 to 25 million years ago. After its uplift, the chain experienced intense erosion and isostatic readjustments. A cross-section through the chain shows an asymmetric flower-like structure with steeper dips on the French side. The Pyrenees are not solely the result of compressional forces, but also show an important sinistral shearing. Geographic arrangement The Pyrenees ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Pic De Bugarach
The Pic de Bugarach () or Pech de Bugarach () (''puèg de Bugarag'' in Occitan, i.e. "Peak of Bugarag") is the highest summit (1230 m) in the Corbières Massif in the French ''Midi''. The western part of the mountain is located on the territory of the commune of Bugarach. Its eastern part is on the territory of Camps-sur-l'Agly. The geology of the Pic de Bugarach is striking. Its top layer is an overthrust from the Iberian plate and is older than the bottom ones. This has given rise to its description as an "upside-down mountain". It is possible to climb up the Bugarach: a classical route called "Voie de la fenêtre" because of a big hole in a cliff, climbs the South face. One may go down via the easiest route, North, and join the "Col de Linas". Climbing still requires a good physical condition, and the mountain has claimed the life of at least one unprepared tourist. Esoterics Due to the mountain's unusual geology, a number of New Agers (called "esoterics" by local re ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Mediterranean Vegetation
Mediterranean forests, woodlands, and scrub is a biome defined by the World Wide Fund for Nature. The biome is generally characterized by dry summers and rainy winters, although in some areas rainfall may be uniform. Summers are typically hot in low-lying inland locations but can be cool near colder seas. Winters are typically mild to cool in low-lying locations but can be cold in inland and higher locations. All these ecoregions are highly distinctive, collectively harboring 10% of the Earth's plant species. Distribution The Mediterranean forests, woodlands, and scrub biome mostly occurs in, but not limited to, the Mediterranean climate zones, in the mid-latitudes: *the Mediterranean Basin *the Chilean Matorral *the California chaparral and woodlands ecoregion of California and the Baja California Peninsula *the Western Cape of South Africa *the southwest and southern Australia. The biome is not limited to the Mediterranean climate zone. It can also be present in other cl ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Mediterranean Sea
The Mediterranean Sea is a sea connected to the Atlantic Ocean, surrounded by the Mediterranean Basin and almost completely enclosed by land: on the north by Western and Southern Europe and Anatolia, on the south by North Africa, and on the east by the Levant. The Sea has played a central role in the history of Western civilization. Geological evidence indicates that around 5.9 million years ago, the Mediterranean was cut off from the Atlantic and was partly or completely desiccated over a period of some 600,000 years during the Messinian salinity crisis before being refilled by the Zanclean flood about 5.3 million years ago. The Mediterranean Sea covers an area of about , representing 0.7% of the global ocean surface, but its connection to the Atlantic via the Strait of Gibraltar—the narrow strait that connects the Atlantic Ocean to the Mediterranean Sea and separates the Iberian Peninsula in Europe from Morocco in Africa—is only wide. The Mediterranean ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Agly
The Agly (; ca, Aglí; oc, Aglin) is a river in southern France. It is long. Its source is in the hills of the Corbières Massif, near Camps-sur-l'Agly. It flows through Saint-Paul-de-Fenouillet, Estagel, Rivesaltes and Saint-Laurent-de-la-Salanque before it flows into the Mediterranean Sea near Le Barcarès Le Barcarès (; ca, El Barcarès) is a commune in the Pyrénées-Orientales department in southern France bordering the Mediterranean Sea. History During the mid 19th century, Le Barcarès was created as a small fishing village which developed .... Tributaries * Boulzane * Désix * Verdouble References Rivers of France Rivers of Aude Rivers of Pyrénées-Orientales Rivers of Occitania (administrative region) 0Agly {{France-river-stub ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Aude (river)
The Aude (; ; Latin ''Atax'' ) is a river of southern France that is long. Its source is in the Pyrenees mountains then runs to Carcassonne and finally reaches the Mediterranean Sea near Narbonne. The river is navigable by raft or canoe for nearly all of its length. It is registered as essential to the Languedoc-Roussillon region. The river gave its name to the Aude '' department''. Etymology In antiquity, the ''Aude'' was called ''Atax'' by the Romans. Some authors in antiquity called the river ''Narbôn'' (e.g. Polybius). In 1342 the Roussillon Cartulary of Alart called it the ''Auda'' or the ''Ribera d'Aude''.Jacques Amiel, ''L'AUDE. Fleuve du pays cathare'', Les presses du Languedoc, Montpellier, 1999 , p. 21. In the Middle Ages the terms ''Adice'', again ''Atax'', ''Fluvium Atacis'', ''Flumine Atace'', ''Flumen Ataze'', and ''Juxta Aditum fluvium'' were also used to designate the Aude. In all likelihood the current name comes from a gradual evolution of ''Atax'' given by S ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Pyrénées-Orientales
Pyrénées-Orientales (; ca, Pirineus Orientals ; oc, Pirenèus Orientals ; ), also known as Northern Catalonia, is a department of the region of Occitania, Southern France, adjacent to the northern Spanish frontier and the Mediterranean Sea. It also surrounds the tiny Spanish exclave of Llívia, and thus has two distinct borders with Spain. In 2019, it had a population of 479,979.Populations légales 2019: 66 Pyrénées-Orientales INSEE Some parts of the Pyrénées-Orientales (like the Cerdagne) are part of the . It is named after the [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Aude
Aude (; ) is a department in Southern France, located in the Occitanie region and named after the river Aude. The departmental council also calls it " Cathar Country" (French: ''Pays cathare'') after a group of religious dissidents active in the 12th to 14th centuries. Its prefecture is Carcassonne and its subprefectures are Limoux and Narbonne. As of 2019, it had a population of 374,070.Populations légales 2019: 11 Aude INSEE Aude is a frequent feminine French given name in Francophone countries, deriving initially from Aude or Oda, a wife of Bertrand, Duke of Aquitaine, and mother of Eudo, brother of Saint Hub ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |