Sierra Vicuña Mackenna
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Sierra Vicuña Mackenna
The Cordillera Vicuña Mackenna is the highest section of the Chilean Coast Range located in northern Chile, west of Pampa del Tamarugal. Its peak reaches over 3000 meters. International Geographical Union, Unesco, Peru. Ministerio de Agricultura. It runs north-south for approximately 170 km parallel to the Andes. The driest parts of Atacama Desert The Atacama Desert ( es, Desierto de Atacama) is a desert plateau in South America covering a 1,600 km (990 mi) strip of land on the Pacific coast, west of the Andes Mountains. The Atacama Desert is the driest nonpolar desert in th ... are located east of the range due to the rain shadow produced by it. The range is named after historian Benjamín Vicuña Mackenna. See also * Vicuña Mackenna Batholith References Chilean Coast Range Landforms of Antofagasta Region Vicuna Mackenna {{Antofagasta-geo-stub ...
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Cerro Armazones
Cerro Armazones is a mountain located in the Sierra Vicuña Mackenna of the Chilean Coast Range, approximately south-east of Antofagasta in the Antofagasta Region, Chile. Before construction started on the European Extremely Large Telescope, the summit was a horizontal control point with an elevation of . The new elevation is . It is located in a privileged zone for optical astronomy because it has 89% cloudless nights a year. It currently hosts the Hexapod-Telescope and other telescopes at the Cerro Armazones Observatory. On 26 April 2010, the European Southern Observatory Council selected Cerro Armazones as the site for the planned Extremely Large Telescope, and construction began in June 2014. Gallery File:Supermoon beckons in the new year.jpg, Supermoon rising up from behind Cerro Armazones. File:Cerro Armazones night-time panorama.jpg, Night-time panorama of Cerro Armazones File:Carving a Route to Armazones.jpg, Carving a route to Armazones, with Cerro Paranal and th ...
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Chilean Coast Range
The Chilean Coastal Range ( es, Cordillera de la Costa) is a mountain range that runs from north to south along the Pacific coast of South America parallel to the Andean Mountains, extending from Morro de Arica in the north to Taitao Peninsula, where it ends at the Chile Triple Junction, in the south. The range has a strong influence on the climate of Chile since it produces a rain shadow to the east. Because of this the vegetation growing on the seaward slopes is much more exuberant than in the interior. Compared to the coastal lowlands and the Intermediate Depression, it is sparsely populated with land use varying from protected areas to grazing and silviculture. The range is present in all Chilean regions, except for Coquimbo Region and Magallanes Region. Geography Like the Andes, the coastal range becomes progressively lower with increasing latitude. The range begins at Morro de Arica in the north and reaches its highest point, of 3114 m, in Sierra Vicuña Mackenna in the ...
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Cerro Vicuña Mackenna
Cerro Vicuña Mackenna is the highest point in the Sierra Vicuña Mackenna and the Chilean Coast Ranges. The peak has a stark desert climate, typical of the Atacama Desert The Atacama Desert ( es, Desierto de Atacama) is a desert plateau in South America covering a 1,600 km (990 mi) strip of land on the Pacific coast, west of the Andes Mountains. The Atacama Desert is the driest nonpolar desert in th .... The peak is named after Benjamín Vicuña Mackenna. References {{DEFAULTSORT:Cerro Vicuna Mackenna Landforms of Antofagasta Region Vicuna Mackenna ...
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Chile
Chile, officially the Republic of Chile, is a country in the western part of South America. It is the southernmost country in the world, and the closest to Antarctica, occupying a long and narrow strip of land between the Andes to the east and the Pacific Ocean to the west. Chile covers an area of , with a population of 17.5 million as of 2017. It shares land borders with Peru to the north, Bolivia to the north-east, Argentina to the east, and the Drake Passage in the far south. Chile also controls the Pacific islands of Juan Fernández, Isla Salas y Gómez, Desventuradas, and Easter Island in Oceania. It also claims about of Antarctica under the Chilean Antarctic Territory. The country's capital and largest city is Santiago, and its national language is Spanish. Spain conquered and colonized the region in the mid-16th century, replacing Inca rule, but failing to conquer the independent Mapuche who inhabited what is now south-central Chile. In 1818, after declaring ...
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Pampa Del Tamarugal
Pampa del Tamarugal ("Plateau of the Tamarugal") is a vast plain encompassing a significant portion of the Norte Grande, Chile, and originally named for the '' Prosopis tamarugo'' trees that used to cover its surface. It is located between the parallels 19°30’ and 22°15’ south latitude and is considered part of the Atacama Desert. It is bounded on the west by the Chilean Coastal Range and on the east by the western slopes of the Andes. The plain occupies a surface area of 12,500 km2 with an average elevation of 1,100 m. Tourism Among the major tourist attractions in the Pampa del Tamarugal are the world heritage site Humberstone and Santa Laura Saltpeter Works, the town of La Tirana, and the Pampa del Tamarugal National Reserve. Gallery File:Pampa del Tamarugal 3.jpg, A modern forest in Pampa del Tamarugal as seen from Chile Route 5 File:Pintados2.jpg, Pre-Hispanic geoglyph A geoglyph is a large design or motif (generally longer than 4 metres) produced on the g ...
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Andes
The Andes, Andes Mountains or Andean Mountains (; ) are the longest continental mountain range in the world, forming a continuous highland along the western edge of South America. The range is long, wide (widest between 18°S – 20°S latitude), and has an average height of about . The Andes extend from north to south through seven South American countries: Venezuela, Colombia, Ecuador, Peru, Bolivia, Chile, and Argentina. Along their length, the Andes are split into several ranges, separated by intermediate depressions. The Andes are the location of several high plateaus—some of which host major cities such as Quito, Bogotá, Cali, Arequipa, Medellín, Bucaramanga, Sucre, Mérida, El Alto and La Paz. The Altiplano plateau is the world's second-highest after the Tibetan plateau. These ranges are in turn grouped into three major divisions based on climate: the Tropical Andes, the Dry Andes, and the Wet Andes. The Andes Mountains are the highest m ...
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Atacama Desert
The Atacama Desert ( es, Desierto de Atacama) is a desert plateau in South America covering a 1,600 km (990 mi) strip of land on the Pacific coast, west of the Andes Mountains. The Atacama Desert is the driest nonpolar desert in the world, and the second driest overall, just behind some very specific spots within the McMurdo Dry Valleys as well as the only hot true desert to receive less precipitation than the polar deserts, and the largest fog desert in the world. Both regions have been used as experimentation sites on Earth for Mars expedition simulations. The Atacama Desert occupies , or if the barren lower slopes of the Andes are included. Most of the desert is composed of stony terrain, salt lakes (''salares''), sand, and felsic lava that flows towards the Andes. The desert owes its extreme aridity to a constant temperature inversion due to the cool north-flowing Humboldt ocean current and to the presence of the strong Pacific anticyclone. The most arid r ...
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Rain Shadow
A rain shadow is an area of significantly reduced rainfall behind a mountainous region, on the side facing away from prevailing winds, known as its leeward side. Evaporated moisture from water bodies (such as oceans and large lakes) is carried by the prevailing onshore breezes towards the drier and hotter inland areas. When encountering elevated landforms, the moist air is driven upslope towards the peak, where it expands, cools, and its moisture condenses and starts to precipitate. If the landforms are tall and wide enough, most of the humidity will be lost to precipitation over the windward side (also known as the ''rainward'' side) before ever making it past the top. As the air descends the leeward side of the landforms, it is compressed and heated, producing foehn winds that ''absorb'' moisture downslope and cast a broad "shadow" of dry climate region behind the mountain crests. This climate typically takes the form of shrub–steppe, xeric shrublands or ev ...
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Benjamín Vicuña Mackenna
Benjamín Vicuña Mackenna (August 25, 1831 – January 25, 1886) was a Chilean writer, journalist, historian and politician. Vicuña Mackenna was of Irish and Basque descent. Biography Benjamín Vicuña Mackenna was born in Santiago, the son of Pedro Félix Vicuña and Carmen Mackenna Vicuña, and grandson of General Juan Mackenna, hero of the Chilean War of Independence. He studied in Santiago, and joined the school of law in 1849. From the beginning of his career he contributed to ''La Tribuna'' newspaper, writing political articles. In 1851 he participated in Pedro Urriola's revolution against the government but was taken prisoner during the attack on the headquarters of the Chacabuco Regiment. On 4 July 1851 Vicuña Mackenna and Roberto Souper managed to escape from the prison disguised as women. In 1852 he lived in exile in the United States, and travelled from San Francisco through Mexico and Canada. A year later he studied agronomy in England, and then visited man ...
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Vicuña Mackenna Batholith
The Vicuña Mackenna Batholith ( es, Batolito Vicuña Mackenna) is a group of plutons in the Chilean Coast Range of northern Chile. The plutons of the batholith formed (cooled from magma to rock) between the Early Jurassic and the Late Cretaceous (192–98 Ma). The magmas that formed the batholith originated in Earth's mantle and have not suffered any significant crustal contamination. A group of Early Cretaceous plutons were intruded syn-tectonically on the Atacama Fault. Subdivision Geologists Miguel Hervé and Nicolás Marinivic identify six major units. From the oldest to the youngest these are: * Barazate Unit (192-181 Ma) * Paranal Unit (ca. 170 Ma). This unit has the largest areal extent. It is composed of gabbronorite, gabbro, diorite, monzodiorite, monzogabbro Monzogabbro is an intrusive rock with a composition intermediate between gabbro and monzonite. It is defined in the QAPF classification as coarse-grained igneous rock in which quartz Quartz is a hard, crys ...
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Landforms Of Antofagasta Region
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 ...
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