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Surco Intrabético
The Intrabaetic Basin ( es, Surco Intrabético or ''Depresión Intrabética'') is a discontinuous series of valleys in the Baetic System of Andalusia, Spain. Description The Intrabaetic Basin is a series of intermontane basins that separate the Penibaetic System to its south from the Subbaetic System to the north. These basins run more or less parallel to the Mediterranean coast. Together, these valleys constitute a route from western Andalusia and the valley of the Guadalquivir to the Spanish Levante, the eastern Mediterranean coastal region of Spain. From west to east, the basins of the Depression of Ronda, the Hoya of Antequera, the Depression of Granada, the Hoya of Guadix, the Hoya of Baza, the Hoya of Huéscar, and the Hoya of Lorca. The valleys of the Intrabaetic Basin stand in contrast to the adjacent mountain ridges that define their collective border and the rocky spurs—formed of limestone, and yielding a dry, nearly treeless landscape—that separate them from on ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Surco Intrabético
The Intrabaetic Basin ( es, Surco Intrabético or ''Depresión Intrabética'') is a discontinuous series of valleys in the Baetic System of Andalusia, Spain. Description The Intrabaetic Basin is a series of intermontane basins that separate the Penibaetic System to its south from the Subbaetic System to the north. These basins run more or less parallel to the Mediterranean coast. Together, these valleys constitute a route from western Andalusia and the valley of the Guadalquivir to the Spanish Levante, the eastern Mediterranean coastal region of Spain. From west to east, the basins of the Depression of Ronda, the Hoya of Antequera, the Depression of Granada, the Hoya of Guadix, the Hoya of Baza, the Hoya of Huéscar, and the Hoya of Lorca. The valleys of the Intrabaetic Basin stand in contrast to the adjacent mountain ridges that define their collective border and the rocky spurs—formed of limestone, and yielding a dry, nearly treeless landscape—that separate them from on ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hoya Of Lorca
Hoya may refer to: Places *Hoya, Germany, a city in Lower Saxony, Germany *County of Hoya, a former state in present Germany * Hoya, Tokyo, now incorporated within Nishi-tokyo, Tokyo, Japan * Hoya, Hpruso, a place in Hpruso Township, Kayah, Myanmar * Hoya, Spain, a hamlet in Lorca, Spain * Hoya, Zimbabwe, a ward of Zimbabwe Other uses * ''Hoya'' (plant), a genus of flowering plants *Hoya (singer), a former member of the South Korean band Infinite *Hoya Corporation, a Japanese company that manufactures optical equipment *''The Hoya'', a campus newspaper at Georgetown University *Georgetown Hoyas, the athletic teams of Georgetown University *Sea pineapple or , a species of edible sea squirt *Hoya (speed cubing method), a method to solve a 4x4x4, 5x5x5 and other big cubes. See also *Heuer *Hoia (other) *Hoya Saxa Hoya Saxa ( ) is the official cheer and "college yell" of Georgetown University and its athletics teams. The term is an Ancient Greek word usually translite ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Granada
Granada (,, DIN 31635, DIN: ; grc, Ἐλιβύργη, Elibýrgē; la, Illiberis or . ) is the capital city of the province of Granada, in the autonomous communities of Spain, autonomous community of Andalusia, Spain. Granada is located at the foot of the Sierra Nevada (Spain), Sierra Nevada mountains, at the confluence of four rivers, the Darro (river), Darro, the Genil, the Monachil (river), Monachil and the Beiro. Ascribed to the Vega de Granada ''comarca'', the city sits at an average elevation of Above mean sea level, above sea level, yet is only one hour by car from the Mediterranean coast, the Costa Tropical. Nearby is the Sierra Nevada Ski Station, where the FIS Alpine World Ski Championships 1996 were held. In the 2021 national census, the population of the city of Granada proper was 227,383, and the population of the entire municipal area was estimated to be 231,775, ranking as the Ranked lists of Spanish municipalities, 20th-largest urban area of Spain. About 3.3% of t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Antequera
Antequera () is a city and municipality in the Comarca de Antequera, province of Málaga, part of the Spanish autonomous community of Andalusia. It is known as "the heart of Andalusia" (''el corazón de Andalucía'') because of its central location among Málaga, Granada, Córdoba, and Seville. The Antequera Dolmens Site is a UNESCO World Heritage site. In 2011, Antequera had a population of 41,854. It covers an area of 749.34 km2 with a population density of 55.85 inhabitants/km2, and is situated at an altitude of 575 meters. Antequera is the most populous city in the interior of the province and the largest in area. It is the twenty-second largest in Spain. The city is located 45 km from Málaga and 115 km from Córdoba. The cities are connected by a high-speed train and the A-45 motorway. Antequera is 160 km from Seville and 102 km from Granada, which is connected by motorway A-92 and will be connected by the high-speed Transverse Axis Rail in th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Almería
Almería (, , ) is a city and municipality of Spain, located in Andalusia. It is the capital of the province of the same name. It lies on southeastern Iberia on the Mediterranean Sea. Caliph Abd al-Rahman III founded the city in 955. The city grew wealthy during the Islamic era, becoming a world city throughout the 11th and 12th centuries. It enjoyed an active port that traded silk, oil and raisins. Etymology The name "Almería" comes from the city's former Arabic name, ''Madīnat al-Mariyya'', meaning "city of the watchtower". As the settlement was originally port or coastal suburb of Pechina, it was initially known as ''Mariyyat al-Bajjāna'' (''Bajjāna'' being the Arabic name for Pechina). History The origin of Almería is connected to the 9th-century establishment of the so-called Republic of Pechina (Bajjana) some kilometres to the north, which was for a time autonomous from the Cordobese central authority: the settlement of current-day Almería initially developed as ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Seville
Seville (; es, Sevilla, ) is the capital and largest city of the Spanish autonomous community of Andalusia and the province of Seville. It is situated on the lower reaches of the River Guadalquivir, in the southwest of the Iberian Peninsula. Seville has a municipal population of about 685,000 , and a metropolitan population of about 1.5 million, making it the largest city in Andalusia, the fourth-largest city in Spain and the 26th most populous municipality in the European Union. Its old town, with an area of , contains three UNESCO World Heritage Sites: the Alcázar palace complex, the Cathedral and the General Archive of the Indies. The Seville harbour, located about from the Atlantic Ocean, is the only river port in Spain. The capital of Andalusia features hot temperatures in the summer, with daily maximums routinely above in July and August. Seville was founded as the Roman city of . Known as ''Ishbiliyah'' after the Islamic conquest in 711, Seville became ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Autovía A-92
The Autovía A-92 is a highway in Andalusia, Spain. It is a major east–west route running south of the Sierra Nevada and is known as the Carretera Sevilla a Granada and Autovía de Andalucía. It starts in Seville heading parallel to the Rio Guadaira to Antequera, where it is crossed by the Autovía A-45 from Málaga to Córdoba. It then crosses the Sierra Gorda to Loja and Vega de Granada before reaching Granada. Here the road is crossed by the Autovía A-44 from the coast and Motril to Jaén. The A-92 then passes over the Puerto de la Mora de Huétor (1,390 m) to Guadix. At Guadix the road branches in two; the south passing La Calahorra Castle and along the Rio Nacimiento to Tabernas and Almería. The northern branch heads along the Hoya de Guadix and the Sierra de Baza before joining the Autovía A-7 at junction 578 km, 17 km south of Lorca. In Murcia the road is numbered Autovía A-91. Over the past many years the road has experienced several problems. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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] |
Sedimentary Basin
Sedimentary basins are region-scale depressions of the Earth's crust where subsidence has occurred and a thick sequence of sediments have accumulated to form a large three-dimensional body of sedimentary rock. They form when long-term subsidence creates a regional depression that provides Accommodation (geology), accommodation space for accumulation of sediments. Over millions or tens or hundreds of millions of years the deposition of sediment, primarily gravity-driven transportation of water-borne eroded material, acts to fill the depression. As the sediments are buried, they are subject to increasing pressure and begin the processes of compaction (geology), compaction and lithification that transform them into sedimentary rock. Sedimentary basins are created by deformation of Earth's lithosphere in diverse geological settings, usually as a result of plate tectonics, plate tectonic activity. Mechanisms of crustal deformation that lead to subsidence and sedimentary basin formati ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Miocene
The Miocene ( ) is the first geological epoch of the Neogene Period and extends from about (Ma). The Miocene was named by Scottish geologist Charles Lyell; the name comes from the Greek words (', "less") and (', "new") and means "less recent" because it has 18% fewer modern marine invertebrates than the Pliocene has. The Miocene is preceded by the Oligocene and is followed by the Pliocene. As Earth went from the Oligocene through the Miocene and into the Pliocene, the climate slowly cooled towards a series of ice ages. The Miocene boundaries are not marked by a single distinct global event but consist rather of regionally defined boundaries between the warmer Oligocene and the cooler Pliocene Epoch. During the Early Miocene, the Arabian Peninsula collided with Eurasia, severing the connection between the Mediterranean and Indian Ocean, and allowing a faunal interchange to occur between Eurasia and Africa, including the dispersal of proboscideans into Eurasia. During the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Conglomerate (geology)
Conglomerate () is a clastic sedimentary rock that is composed of a substantial fraction of rounded to subangular gravel-size clasts. A conglomerate typically contains a matrix of finer-grained sediments, such as sand, silt, or clay, which fills the interstices between the clasts. The clasts and matrix are typically cemented by calcium carbonate, iron oxide, silica, or hardened clay. Conglomerates form by the consolidation and lithification of gravel. They can be found in sedimentary rock sequences of all ages but probably make up less than 1 percent by weight of all sedimentary rocks. In terms of origin and depositional mechanisms, they are closely related to sandstones and exhibit many of the same types of sedimentary structures, e.g., tabular and trough cross-bedding and graded bedding.Boggs, S. (2006) ''Principles of Sedimentology and Stratigraphy.'', 2nd ed. Prentice Hall, New York. 662 pp. Friedman, G.M. (2003) ''Classification of sediments and sedimentary rocks.'' In G ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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