Sistema Bético
The Baetic System or Betic System ( es, Sistema Bético) is one of the main systems of mountain ranges in Spain. Located in the southern and eastern Iberian Peninsula, it is also known as the Cordilleras Béticas (Baetic Mountain Ranges) or Baetic Mountains. The name of the mountain system derives from the ancient Roman region of Baetica, one of the Imperial Roman provinces of ancient Hispania. Geography The Baetic System is made up of multiple mountain ranges that reach from western Andalusia to the Region of Murcia, southern Castile-La Mancha and the Land of Valencia. To the north, the Baetic Ranges are separated from the Meseta Central and the Sierra Morena by the basin of the Guadalquivir. The Iberian System rises north of the eastern part of the Prebaetic System, the northernmost prolongation of the Baetic System. Generally the mountain ranges that are part of this system are aligned in a southwest-northeast direction. The most well-known range of the Baetic System is th ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Mulhacén
Mulhacén (), with an elevation of , is the highest mountain in peninsular Spain and in all of the Iberian Peninsula. It is part of the Sierra Nevada range in the Cordillera Penibética. It is named after Abu l-Hasan Ali, known as ''Muley Hacén'' in Spanish, the penultimate Muslim King of Granada in the 15th century who, according to legend, was buried on the summit of the mountain. Mulhacén is the highest peak in Western EuropeThe Canary Islands and Greenland, which are politically attached to Europe, but which are geographically part of Africa and North America respectively, have higher peaks. outside of the Alps. It is also the third-most topographically prominent peak in Western Europe, after Mont Blanc and Mount Etna, and is ranked 64th in the world by prominence. The peak is not exceptionally dramatic in terms of steepness or local relief. The south flank of the mountain is gentle and presents no technical challenge, as is the case for the long west ridge. The shorter, s ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Baetica
Hispania Baetica, often abbreviated Baetica, was one of three Roman provinces in Hispania (the Iberian Peninsula). Baetica was bordered to the west by Lusitania, and to the northeast by Hispania Tarraconensis. Baetica remained one of the basic divisions of Hispania under the Visigoths down to 711. Baetica was part of Al-Andalus under the Arabs in the 8th century and approximately corresponds to modern Andalusia. Name In Latin, ' is an adjectival form of ', the Roman name for the Guadalquivir River, whose fertile valley formed one of the most important parts of the province. History Before Romanization, the mountainous area that was to become Baetica was occupied by several settled Iberian tribal groups. Celtic influence was not as strong as it was in the Celtiberian north. According to the geographer Claudius Ptolemy, the indigenes were the powerful Turdetani, in the valley of the Guadalquivir in the west, bordering on Lusitania, and the partly Hellenized Turduli with the ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Gibraltar Arc
The Gibraltar Arc is a geological region corresponding to an arcuate orogen surrounding the Alboran Sea, between the Iberian Peninsula and Africa. It consists of the Betic Cordillera (south Spain), and the Rif (North Morocco). The Gibraltar Arc is located at the western end of the Mediterranean Alpine belt and formed during the Neogene due to convergence of the Eurasian and African plates. Maximum altitudes of the region are reached at the Mulhacén peak at the Cordillera Betica. Precipitation is collected mainly by the Guadalquivir (Betics) and Sebou (Rif) rivers, which have delivered most sedimentary infill of the homonym sedimentary foreland basins.. Tectonic evolution North–south convergence of the Eurasian and African plates occurred during the middle Oligocene to the late Miocene, followed by northwest–southeast convergence from the late Tortonian to present. The Gibraltar Arc was formed during the Neogene due to a combination of western migration of the orogenic mount ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Orogeny
Orogeny is a mountain building process. An orogeny is an event that takes place at a convergent plate margin when plate motion compresses the margin. An ''orogenic belt'' or ''orogen'' develops as the compressed plate crumples and is uplifted to form one or more mountain ranges. This involves a series of geological processes collectively called orogenesis. These include both structural deformation of existing continental crust and the creation of new continental crust through volcanism. Magma rising in the orogen carries less dense material upwards while leaving more dense material behind, resulting in compositional differentiation of Earth's lithosphere ( crust and uppermost mantle). A synorogenic process or event is one that occurs during an orogeny. The word "orogeny" () comes from Ancient Greek (, , + , , ). Although it was used before him, the term was employed by the American geologist G. K. Gilbert in 1890 to describe the process of mountain-building as distinguished f ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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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]   |
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Cabo De Gata
Cabo de Gata is a cape located in Níjar, Almería in the south of Spain, one of the biggest capes. It is the driest place in the Iberian Peninsula (150-170 mm average precipitation, being the lowest 52 mm in 1981). However, the area that it occupies is not considered a desert, even though there is one nearby: the Tabernas Desert, located 30 km in a northwest direction. The lowest temperature registered in Cabo de Gata was 0.1 °C. San José, Las Negras, Agua Amarga, Isleta del Moro, Rodalquilar, San Miguel, Almadraba de Moteleva, Fernán Pérez, Las Hortichuelas, Pozo de los Frailes, Los Escullos, Níjar and Carboneras are towns found in Cabo de Gata. The lighthouse is a famous landmark. On 26 March 2008 it was declared Parque Natural. References External links * {{commons-inline Geography of the Province of Almería Gata Davionte Ganter, known professionally as GaTa, is an American rapper and actor known for his role in the FXX TV series ''Dave'', ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Sierra Nevada (Spain)
Sierra Nevada (; meaning "mountain range covered in snow") is a mountain range in the Andalusian province of Granada in Spain. It contains the highest point of continental Spain:The highest peak in Spanish territory is Teide on the island of Tenerife in the Canary Islands, which is politically Spanish but geographically part of Africa. Mulhacén, at above sea level. It is a popular tourist destination, as its high peaks make skiing possible in one of Europe's most southerly ski resorts, in an area along the Mediterranean Sea predominantly known for its warm temperatures and abundant sunshine. At its foothills is found the city of Granada, and a little further south, Almería and Málaga. Parts of the range have been included in the Sierra Nevada National Park. The range has also been declared a biosphere reserve. The Sierra Nevada Observatory and the IRAM radiotelescope are located on the northern slopes at an elevation of . Formation The Sierra Nevada was formed during the ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Prebaetic System
The Prebaetic System ( es, Sistemas Prebéticos or ''Sistema Prebético'', also often referred to simply as ''Prebético'') is a system of mountain ranges that forms the northeasternmost prolongation of the Baetic System in the southern Iberian Peninsula. Geography Although it is sometimes referred to as ''Cordillera Prebética'', it is not a proper cordillera, or continuous alignment of ranges, but a broken system of mountain ranges. Unlike the other two subsystems of the Baetic System, it is not present in the western area, but begins west of the eastern edge of the Sierra Sur de Jaén near Martos. The Prebaetic System runs along eastern interior Andalusia, across the Region of Murcia, reaching the Mediterranean Sea shores in the southern Valencian Community. Its highest point is La Sagra, Sierra de la Sagra; other high ranges are Sierra de Segura and Sierra de Cazorla. The Sierra de María in northern Almeria Province runs across the Prebaetic and the Penibaetic System, over ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Guadalquivir
The Guadalquivir (, also , , ) is the fifth-longest river in the Iberian Peninsula and the second-longest river with its entire length in Spain. The Guadalquivir is the only major navigable river in Spain. Currently it is navigable from the Gulf of Cádiz to Seville, but in Roman times it was navigable to Córdoba. Geography The river is long and drains an area of about . It rises at Cañada de las Fuentes (village of Quesada) in the Cazorla mountain range ( Jaén), flows through Córdoba and Seville and reaches the sea at the fishing village of Bonanza, in Sanlúcar de Barrameda, flowing into the Gulf of Cádiz, in the Atlantic Ocean. The marshy lowlands at the river's mouth are known as " Las Marismas". The river borders the Doñana National Park reserve. Name The modern name of Guadalquivir comes from the Arabic ''al-wādī l-kabīr'' (), meaning "the big river". There was a variety of names for the Guadalquivir in Classical and pre-Classical times. According to Titus ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Sierra Morena
The Sierra Morena is one of the main systems of mountain ranges in Spain. It stretches for 450 kilometres from east to west across the south of the Iberian Peninsula, forming the southern border of the ''Meseta Central'' plateau and providing the watershed between the valleys of the Guadiana to the north and the west, and the Guadalquivir to the south. Its highest summit is 1,332 m high Bañuela. Other notable peaks are Corral de Borros 1,312 m and Cerro de la Estrella 1,298 m. The name ''Sierra Morena'' has a strong legendary reputation in Spanish culture and tradition, with myths about bandits ''(Los bandidos de Sierra Morena)'', a giant snake ''(El Saetón de Sierra Morena)'' and a child brought up by wolves (Marcos Rodríguez Pantoja), among others. This range is also mentioned in the famous Mexican song "Cielito Lindo" and in one of the most well known traditional Spanish songs, "Soy Minero", interpreted by Antonio Molina. Description The Sierra Morena stretches f ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Meseta Central
The ''Meseta Central'' (, sometimes referred to in English as Inner Plateau) is one of the basic geographical units of the Iberian Peninsula. It consists of a plateau covering a large part of the latter's interior. Developed during the 19th century, the concept of ''meseta central'' was handled by Heinrich Moritz Willkomm in lower case, and eventually was reportedly the first in using it in upper case, giving it a toponymic nature. The concept was also brought forward by José Macpherson y Hemas, while the writers of the Spanish Generation of '98 greatly contributed to its popularisation among the public sphere. The Sistema Central mountain range cuts across the Meseta Central, leaving the ''Submeseta Norte'' sub-unit (with heights mostly ranging from 700 to 800 m) to the North and the ''Submeseta Sur'' (with heights mostly ranging from 600 to 700 m) to the South. Respectively, the former is drained by the Douro while the latter is drained by the Tagus and the Guadiana. The ''m ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Valencia (autonomous Community)
The Valencian Community ( ca-valencia, Comunitat Valenciana, es, Comunidad Valenciana) is an Autonomous communities of Spain, autonomous community of Spain. It is the fourth most populous Spanish Autonomous communities of Spain, autonomous community after Andalusia, Catalonia and the Community of Madrid with more than five million inhabitants.Instituto Nacional de Estadística, Madrid, 2020. Its homonymous capital Valencia is the third largest city and metropolitan area in Spain. It is located along the Mediterranean Sea, Mediterranean coast on the east side of the Iberian Peninsula. It borders with Catalonia to the north, Aragon and Castilla–La Mancha to the west, and Region of Murcia, Murcia to the south, and the Balearic Islands are to its east. The Valencian Community consists of three Provinces of Spain, provinces which are province of Castellón, Castellón, province of Valencia, Valencia and province of Alicante, Alicante. According to Valencia's Statute of Autonomy, th ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |