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La Cadena
La Cadena is a mountain in the Frigiliana municipality of the Province of Málaga in southern Spain, in the Sierra de Almijara. Location La Cadena is one of the main peaks of the Sierras of Tejeda, Almijara and Alhama Natural Park. The peak of La Cadena has an elevation of . To reach the peak a climber must walk along a very narrow ridge with sections no more than wide and sections that are very broken. The rocks are firm, but may be slippery and dangerous if they are wet or icy. At the summit there is a hunting reserve sign and a small iron cross, both well-embedded in the rock. Geology The Sierra de Almijara is a rough mass of marble mountains with sharp ridges that stretches east from the Puerto de Cómpeta. The mountains contain narrow ridges separated by deep valleys cut by the streams and rivers, resulting in many small sub-basins. All of the park has the calcareous formations of the Subbética region, with marbles, shales, phyllites, etc. The area is rich in quartzite ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cerro Del Lucero
The Cerro del Lucero, also known as El Lucero, Raspón de los Moriscos or Cerro de los Moriscos, is a mountain in the Alhama de Granada municipality of the Province of Granada in southern Spain, in the Sierra Almijara. Location The Cerro del Lucero is in the Sierras of Tejeda, Almijara and Alhama Natural Park. The Sierra Almijara is a rough mass of marble mountains with sharp ridges that stretched east from the Puerto de Cómpeta. The most prominent peak is the Cerro Lucero. The mountain has an elevation of , and the peak has a Topographic prominence, prominence of . The peak is from Navachica () in an ESE direction and from La Maroma ( in a WNW direction. Access The Cerro del Lucero is on the border between Malaga and Granada, and can be accessed from both provinces. The peak can be accessed from the La Resinera information point, heading south for about along a path to the start of the trail. From here a trail with high difficulty leads to the peak. Peak The Cerro del L ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Calcareous
Calcareous () is an adjective meaning "mostly or partly composed of calcium carbonate", in other words, containing lime or being chalky. The term is used in a wide variety of scientific disciplines. In zoology ''Calcareous'' is used as an adjectival term applied to anatomical structures which are made primarily of calcium carbonate, in animals such as gastropods, i.e., snails, specifically about such structures as the operculum, the clausilium, and the love dart. The term also applies to the calcium carbonate tests of often more or less microscopic Foraminifera. Not all tests are calcareous; diatoms and radiolaria have siliceous tests. The molluscs are calcareous, as are calcareous sponges ( Porifera), that have spicules which are made of calcium carbonate. In botany ''Calcareous grassland'' is a form of grassland characteristic of soils containing much calcium carbonate from underlying chalk or limestone rock. In medicine The term is used in pathology, for example i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gneiss
Gneiss ( ) is a common and widely distributed type of metamorphic rock. It is formed by high-temperature and high-pressure metamorphic processes acting on formations composed of igneous or sedimentary rocks. Gneiss forms at higher temperatures and pressures than schist. Gneiss nearly always shows a banded texture characterized by alternating darker and lighter colored bands and without a distinct cleavage. Gneisses are common in the ancient crust of continental shields. Some of the oldest rocks on Earth are gneisses, such as the Acasta Gneiss. Description Orthogneiss from the Czech Republic In traditional English and North American usage, a gneiss is a coarse-grained metamorphic rock showing compositional banding (gneissic banding) but poorly developed schistosity and indistinct cleavage. In other words, it is a metamorphic rock composed of mineral grains easily seen with the unaided eye, which form obvious compositional layers, but which has only a weak tendency to fracture ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Quartzite
Quartzite is a hard, non- foliated metamorphic rock which was originally pure quartz sandstone.Essentials of Geology, 3rd Edition, Stephen Marshak, p 182 Sandstone is converted into quartzite through heating and pressure usually related to tectonic compression within orogenic belts. Pure quartzite is usually white to grey, though quartzites often occur in various shades of pink and red due to varying amounts of hematite. Other colors, such as yellow, green, blue and orange, are due to other minerals. The term ''quartzite'' is also sometimes used for very hard but unmetamorphosed sandstones that are composed of quartz grains thoroughly cemented with additional quartz. Such sedimentary rock has come to be described as orthoquartzite to distinguish it from metamorphic quartzite, which is sometimes called metaquartzite to emphasize its metamorphic origins. Quartzite is very resistant to chemical weathering and often forms ridges and resistant hilltops. The nearly pure silica conte ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Phyllite
Phyllite ( ) is a type of foliated metamorphic rock created from slate that is further metamorphosed so that very fine grained white mica achieves a preferred orientation.Stephen Marshak ''Essentials of Geology'', 3rd ed. It is primarily composed of quartz, sericite mica, and chlorite. Phyllite has fine-grained mica flakes, whereas slate has extremely fine mica flakes, and schist has large mica flakes, all mica flakes of which have achieved a preferred orientation. Among foliated metamorphic rocks, it represents a gradation in the degree of metamorphism between slate and schist. The minute crystals of graphite, sericite, or chlorite, or the translucent fine-grained white mica, impart a silky, sometimes golden sheen to the surfaces of cleavage, called "phyllitic luster". The word comes from the Greek ''phyllon'', meaning "leaf". The protolith (or parent rock) for phyllite is shale or pelite, or slate, which in turn came from a shale protolith. Its constituent platy minerals ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shale
Shale is a fine-grained, clastic sedimentary rock formed from mud that is a mix of flakes of clay minerals (hydrous aluminium phyllosilicates, e.g. kaolin, Al2 Si2 O5( OH)4) and tiny fragments (silt-sized particles) of other minerals, especially quartz and calcite.Blatt, Harvey and Robert J. Tracy (1996) ''Petrology: Igneous, Sedimentary and Metamorphic'', 2nd ed., Freeman, pp. 281–292 Shale is characterized by its tendency to split into thin layers ( laminae) less than one centimeter in thickness. This property is called '' fissility''. Shale is the most common sedimentary rock. The term ''shale'' is sometimes applied more broadly, as essentially a synonym for mudrock, rather than in the more narrow sense of clay-rich fissile mudrock. Texture Shale typically exhibits varying degrees of fissility. Because of the parallel orientation of clay mineral flakes in shale, it breaks into thin layers, often splintery and usually parallel to the otherwise indistinguishable beddin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Marble
Marble is a metamorphic rock composed of recrystallized carbonate minerals, most commonly calcite or Dolomite (mineral), dolomite. Marble is typically not Foliation (geology), foliated (layered), although there are exceptions. In geology, the term ''marble'' refers to metamorphosed limestone, but its use in stonemasonry more broadly encompasses unmetamorphosed limestone. Marble is commonly used for Marble sculpture, sculpture and as a building material. Etymology The word "marble" derives from the Ancient Greek (), from (), "crystalline rock, shining stone", perhaps from the verb (), "to flash, sparkle, gleam"; Robert S. P. Beekes, R. S. P. Beekes has suggested that a "Pre-Greek origin is probable". This Stem (linguistics), stem is also the ancestor of the English language, English word "marmoreal," meaning "marble-like." While the English term "marble" resembles the French language, French , most other European languages (with words like "marmoreal") more closely resemb ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Subbética
Subbetica is a comarca in the province of Córdoba, Spain. It contains the following municipalities: * Almedinilla * Benamejí * Cabra * Carcabuey * Doña Mencía * Encinas Reales * Fuente-Tójar * Iznájar * Lucena * Luque * Palenciana * Priego de Córdoba * Rute * Zuheros Zuheros is a mountain village located in the province of Córdoba, Spain. According to the 2006 census (INE INE, Ine or ine may refer to: Institutions * Institut für Nukleare Entsorgung, a German nuclear research center * Instituto Nacional de ... References Comarcas of Andalusia Province of Córdoba (Spain) {{Andalusia-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sierras Of Tejeda, Almijara And Alhama Natural Park
The Sierras of Tejeda, Almijara and Alhama Natural Park ( es, Parque natural de las Sierras de Tejeda, Almijara y Alhama) is a protected area in the Spanish provinces of Málaga and Granada. It contains the Sierra de Tejeda and Sierra de Almijara mountains. The park is mountainous and is partly covered by pine forests at the lower levels, while typical Mediterranean vegetation is found higher up. There is a large number of endemic species. Establishment The park was declared on 21 September 1999. The park is designated "''Lugares de Importancia Comunitaria''" (LIC; Places of Community Importance) in Andalusia, "''Zonas de Especial Protección para las Aves''" (ZEPA; Special Protection Areas for Birds) in Andalusia and, "''Parque adherido a la Carta Europea de Turismo Sostenible''" (CETS; Park adhering to the European Charter for Sustainable Tourism). The park was designated a Site of Community Importance (SCI) of the Mediterranean Biogeographic Region by the European Commission ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Andalusia
Andalusia (, ; es, Andalucía ) is the southernmost Autonomous communities of Spain, autonomous community in Peninsular Spain. It is the most populous and the second-largest autonomous community in the country. It is officially recognised as a Nationalities and regions of Spain, "historical nationality". The territory is divided into eight Provinces of Spain, provinces: Province of Almería, Almería, Province of Cádiz, Cádiz, Province of Córdoba (Spain), Córdoba, Province of Granada, Granada, Province of Huelva, Huelva, Province of Jaén (Spain), Jaén, Province of Málaga, Málaga, and Province of Seville, Seville. Its capital city is Seville. The seat of the High Court of Justice of Andalusia is located in the city of Granada. Andalusia is located in the south of the Iberian Peninsula, in southwestern Europe, immediately south of the autonomous communities of Extremadura and Castilla-La Mancha; west of the autonomous community of Region of Murcia, Murcia and the Mediterr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sierra De Almijara
The Sierra de Almijara is a mountain range in the provinces of Granada and Málaga in southern Spain. The rocks are mainly marble, giving a white or gray color to the narrow ridges and deep ravines. The range is mostly protected by the Sierras of Tejeda, Almijara and Alhama Natural Park. Location The Sierras of Tejida and Almijara form a single range about west of the Sierra Nevada. The mountains form a barrier between the coast and the interior. They are part of the Penibaetic System. The Sierras of Tejeda, Almijara and Alhama Natural Park covers . The park contains the Sierra de Tejeda and Sierra de Almijara mountains in the Axarquía ''comarca'' of the eastern province of Málaga and the Alhama ''comarca'' on the southwest of the province of Granada. Topography The Sierra de Almijara is a rough mass of marble mountains with sharp ridges that stretches east from the Puerto de Cómpeta. The mountains contain narrow ridges separated by deep valleys cut by the streams and riv ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Frigiliana
Frigiliana is a town and municipality in the province of Málaga, part of the autonomous community of Andalusia in southern Spain. The municipality is situated approximately 71 kilometers east of Málaga, the provincial capital, and approximately 6 kilometers north of Nerja. It is located in the comarca of La Axarquía, the easternmost region of the province, and integrated into the judicial district of Torrox. Moorish-Mudéjar district This is the old district inhabited by the Moors before and after the ''Reconquista''. Its name Mudéjar is used to describe the architectural style used by Muslim craftsmen working in Christian territory. The quarter is made up of steep cobbled alleyways winding past white houses resplendent with flowers. Culture For four days at the end of August each year, Frigiliana hosts the Festival of the Three Cultures (Festival de las Tres Culturas), celebrating the region's historic confluence and co-existence of Christian, Muslim and Jewish traditions ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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