Sierra De Famatina
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Sierra De Famatina
200px, Coat of arms of La Rioja featuring ''Cerro General Belgrano'' Sierra de Famatina is mountain range and massif in the Andes of the Argentine province of La Rioja La Rioja () is an autonomous community and province in Spain, in the north of the Iberian Peninsula. Its capital is Logroño. Other cities and towns in the province include Calahorra, Arnedo, Alfaro, Haro, Santo Domingo de la Calzada, an .... The range rises between the north-south valleys of Bermejo and Antinaco-Los Colorados. The highest point, designated Cerro General Belgrano (once known as ''Nevado de Famatina''), rises 20,505 ft (6,250 m) and is featured in the coat of arms of La Rioja Province. See also * Famatina Department, La Rioja * Famatinian orogeny * '' Reicheocactus famatimensis'' Landforms of La Rioja Province, Argentina Mountain ranges of Argentina Six-thousanders of the Andes Sierras Pampeanas {{LaRiojaAR-geo-stub ...
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Coat Of Arms Of The La Rioja Province
A coat typically is an outer garment for the upper body as worn by either gender for warmth or fashion. Coats typically have long sleeves and are open down the front and closing by means of buttons, zippers, hook-and-loop fasteners, toggles, a belt, or a combination of some of these. Other possible features include collars, shoulder straps and hoods. Etymology ''Coat'' is one of the earliest clothing category words in English, attested as far back as the early Middle Ages. (''See also'' Clothing terminology.) The Oxford English Dictionary traces ''coat'' in its modern meaning to c. 1300, when it was written ''cote'' or ''cotte''. The word coat stems from Old French and then Latin ''cottus.'' It originates from the Proto-Indo-European word for woolen clothes. An early use of ''coat'' in English is coat of mail (chainmail), a tunic-like garment of metal rings, usually knee- or mid-calf length. History The origins of the Western-style coat can be traced to the sleeved, close- ...
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Mountain Range
A mountain range or hill range is a series of mountains or hills arranged in a line and connected by high ground. A mountain system or mountain belt is a group of mountain ranges with similarity in form, structure, and alignment that have arisen from the same cause, usually an orogeny. Mountain ranges are formed by a variety of geological processes, but most of the significant ones on Earth are the result of plate tectonics. Mountain ranges are also found on many planetary mass objects in the Solar System and are likely a feature of most terrestrial planets. Mountain ranges are usually segmented by highlands or mountain passes and valleys. Individual mountains within the same mountain range do not necessarily have the same geologic structure or petrology. They may be a mix of different orogenic expressions and terranes, for example thrust sheets, uplifted blocks, fold mountains, and volcanic landforms resulting in a variety of rock types. Major ranges Most geolo ...
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Massif
In geology, a massif ( or ) is a section of a planet's crust that is demarcated by faults or flexures. In the movement of the crust, a massif tends to retain its internal structure while being displaced as a whole. The term also refers to a group of mountains formed by such a structure. In mountaineering and climbing literature, a massif is frequently used to denote the main mass of an individual mountain. The massif is a smaller structural unit of the crust than a tectonic plate, and is considered the fourth-largest driving force in geomorphology. The word is taken from French (in which the word also means "massive"), where it is used to refer a large mountain mass or compact group of connected mountains forming an independent portion of a range. One of the most notable European examples of a massif is the Massif Central of the Auvergne region of France. The Face on Mars is an example of an extraterrestrial massif. Massifs may also form underwater, as with the Atlanti ...
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La Rioja Province (Argentina)
La Rioja () is a province of Argentina located in the west of the country. The landscape of the province consist of a series of arid to semi-arid mountain ranges and agricultural valleys in between. It is in one of these valleys that the capital of the province, the city of la La Rioja, lies. Neighboring provinces are from the north clockwise Catamarca, Córdoba, San Luis and San Juan. The dinosaur '' Riojasaurus'' is named after the province. History Petroglyphs created by early indigenous peoples at the Talampaya National Park are dated around 10,000 years BC. Succeeding cultures of indigenous peoples developed here. The Diaguita, Capayan and the Olongasta peoples inhabited the territory of present-day La Rioja Province at the time of encounter with the Spanish colonists in the 16th century. Juan Ramírez de Velazco founded ''Todos Los Santos de la Nueva Rioja'' in 1591 under the government of Tucumán of the Viceroyalty of Peru. In 1630 the Calchaquí people revolted ...
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Nevado De Famatina
Nevado de Famatina (also called Manuel Belgrano) is a peak in Argentina with an elevation of metres. It is the highest point of Sierra de Famatina. It is located within the territory of the Argentinean province of La Rioja. Its slopes are within the administrative boundaries of the Argentinean cities: Famatina and Chilecito. First ascent The first recorded ascent of Famatina was by Rudolf Hauthal (Germany) on 20 May 1895. Elevation Other data from available digital elevation models: SRTM yields 6094 metres, ALOS 6066 metres and TanDEM-X 6124 metres. The height of the nearest key col is 3332 meters, leading to a topographic prominence of 2783 meters. Its topographic dominance is 45.51%, parent peak is Ojos del Salado and the Topographic isolation is 223.1 kilometers The kilometre ( SI symbol: km; or ), spelt kilometer in American English, is a unit of length in the International System of Units (SI), equal to one thousand metres (kilo- being the SI prefix for ). It i ...
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Famatina Department, La Rioja
Famatina is an Argentinian Department in La Rioja Province. Geography The department borders Catamarca Province to the north, San Blas de los Sauces Department, Castro Barros Department and Sanagasta Department to the east, Chilecito Department to the south, Vinchina Department to the west and General Lamadrid Department to the southwest. Population According to estimates for June 2007, the population was 6819 inhabitants.Dirección General de Estadística de la Provincia de La Rioj Department Localities * Famatina * Alto Carrizal * Ángulos * Antinaco * Bajo Carrizal * Campanas * Chañarmuyo * La Cuadra * Pituil * Plaza Vieja * Santa Cruz * Santo Domingo Flora & fauna Endemic Famatina animals are:Ejemplar de Taruka, habitante de la región. Autor: Fernando Falke birds Upucerthia validirostris rufescens, Upucerthia ruficauda famatinae, Cinclodes fuscus riojanus, Asthenes modesta serrana, lizard Liolaemus famatinae (near extinction), Phymaturus mallimacci ( ...
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Famatinian Orogeny
The Famatinian orogeny ( es, Orogenia de Famatina) is an orogeny that predates the rise of the Andes and that took place in what is now western South America during the Paleozoic, leading to the formation of the Famatinian orogen also known as the Famatinian belt. The Famatinian orogeny lasted from the Late Cambrian to at least the Late Devonian and possibly the Early Carboniferous, with orogenic activity peaking about 490 to 460 million years ago. The orogeny involved metamorphism and deformation in the crust and the eruption and intrusion of magma along a Famatinian magmatic arc that formed a chain of volcanoes. The igneous rocks of the Famatinian magmatic arc are of calc-alkaline character and include gabbros, tonalites and granodiorites. The youngest igneous rocks of the arc are granites. The relationship of the orogeny with the Achala and Cerro Aspero batholiths of central Argentina is not fully understood. These Devonian batholiths are possibly of post-orogenic chara ...
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Reicheocactus
''Reicheocactus'', is a monotypic genus of cactus in the family Cactaceae, native to north western Argentina. It has only one known species; ''Reicheocactus famatimensis'' It is usually solitary or slowly clumping and slow growing. The stems are small flattened-roundish to cylindrical with very short spidery-pectinate spines and egg-yellow flowers. The species grows at elevations of metres above sea level. It is found in high altitude grasslands on rocky soils. The species is not common or abundant, however it is difficult to see because of its small size. The major threat for the species is over collection (by plant collectors). The potential development of mining in its natural habitat could affect the populations of the species in the near future. The genus ''Reicheocactus'' was published in Cactaceae (Berlin) 1941(2) on page 76 (published in 1942), and the species was published in Cactaceae Syst. Init. vol.28 on page 30 in 2012. It was once thought to be a synonym of ''Reb ...
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Landforms Of La Rioja Province, Argentina
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, 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. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateaux, and plains are the fo ...
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Mountain Ranges Of Argentina
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited Summit (topography), summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are Monadnock, isolated summits, but most occur in mountain ranges. Mountain formation, Mountains are formed through Tectonic plate, tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through Slump (geology), slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce Alpine climate, colder climates than at sea level at similar latitude. These colder climates strongly affect the Montane ecosystems, ecosys ...
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