Antillanca Group
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Antillanca Group
The Antillanca Group is a volcanic group of scoria cones, maars and small stratovolcanoes, in Chile. Casablanca stratovolcano is the tallest volcano of the group, which shelters the Antillanca ski resort on its west flank. Aguas Calientes and Puyehue Hot springs also form part of this volcanic group. The complex encompasses 380 km2 and to the west is bordered by the lakes Puyehue and Rupanco. A great portion of the Antillanca Group lies within Puyehue National Park. The complex is neighbor of the volcanoes Puyehue, Cordón Caulle Cordón is a central ''barrio'' (neighbourhood or district) of Montevideo, Uruguay, located East of the Centro. Its main avenue is 18 de Julio Avenue. History Cordón was the first neighborhood to be created outside the walls of the old Citade ..., Puntiagudo and Osorno. References Volcanoes of Los Lagos Region Mountains of Chile Stratovolcanoes of Chile Maars of Chile Cinder cones of Chile Volcanic groups {{LosLagos- ...
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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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Rupanco Lake
Rupanco Lake is located in Los Lagos Region of 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 a .... The closest city, Osorno, has a primary school named after it as well. External linksPictures of Rupanco LakeAbout Rupanco Lake
Rupanco Lakes of Los Lagos Region {{LosLagos-geo-stub ...
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Maars Of Chile
A maar is a broad, low-relief volcanic crater caused by a phreatomagmatic eruption (an explosion which occurs when groundwater comes into contact with hot lava or magma). A maar characteristically fills with water to form a relatively shallow crater lake which may also be called a maar. The name comes from a Moselle Franconian dialect word used for the circular lakes of the Daun area of Germany. Notes: * According to German Wikipedia's ''"Maar"'' article, in 1544 in his book ''Cosmographia'', Sebastian Münster (1488–1552) first applied the word "maar" (as ''Marh'') to the Ulmener Maar and the Laacher See. See: Sebastian Münster, ''Cosmographia'' (Basel, Switzerland: Heinrich Petri, 1544)p. 341. From p. 341: ''"Item zwen namhafftiger seen seind in der Eyfel / einer bey de schloß Ulmen / und ein ander bey dem Closter züm Laich / die seind sere tieff / habe kein ynflüß aber vil außflüß / die nennet man Marh unnd seind fischreich."'' (Also two noteworthy lakes are ...
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Stratovolcanoes Of Chile
A stratovolcano, also known as a composite volcano, is a conical volcano built up by many layers (strata) of hardened lava and tephra. Unlike shield volcanoes, stratovolcanoes are characterized by a steep profile with a summit crater and periodic intervals of explosive eruptions and effusive eruptions, although some have collapsed summit craters called calderas. The lava flowing from stratovolcanoes typically cools and hardens before spreading far, due to high viscosity. The magma forming this lava is often felsic, having high-to-intermediate levels of silica (as in rhyolite, dacite, or andesite), with lesser amounts of less-viscous mafic magma. Extensive felsic lava flows are uncommon, but have travelled as far as . Stratovolcanoes are sometimes called composite volcanoes because of their composite stratified structure, built up from sequential outpourings of erupted materials. They are among the most common types of volcanoes, in contrast to the less common shield volcanoe ...
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Mountains Of Chile
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 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 isolated summits, but most occur in mountain ranges. Mountains are formed through 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 slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain ...
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Volcanoes Of Los Lagos Region
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 plates slide ...
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Osorno (volcano)
Osorno Volcano is a tall conical stratovolcano lying between Osorno Province and Llanquihue Province, in Los Lagos Region of Chile. It stands on the southeastern shore of Llanquihue Lake, and also towers over Todos los Santos Lake. Osorno is considered a symbol of the local landscape and, as such, tends to be the referential element of the area in regards to tourism and marks the beginning of Chilean Patagonia. Etymology The current name comes from a nearby town, Osorno, where it was visible to Spanish settlers. Native populations gave it different names, such as Purailla, Purarhue, Prarauque, Peripillan, Choshueco, Hueñauca and Guanauca. The latter two names were the most common in the mid-18th century. Overview The volcano has a height of 2,652 meters (8,701 feet) and its imposing conical feature looms over lake Llanquihue, across from the cities of Frutillar, Puerto Varas, and Llanquehue. There has been no volcanic activity for over one hundred years. Skiing and hiking ...
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Puntiagudo-Cordón Cenizos
Puntiagudo-Cordón Cenizos () is a snow-capped volcanic chain located in the Andes, in Los Lagos Region of Chile, near Volcán Osorno. It lies between Rupanco Lake and Todos los Santos Lake. "Volcán Puntiagudo" (Spanish for "Sharp-pointed volcano") is a stratovolcano with a prominent 2,493 m high sharp-pointed summit that results from glacial dissection and gets its name from this feature. According to locals, the Puntiagudo volcano lost some of its sharp point in the earthquake of 1960 (9.4–9.6 Mw). So the volcano was more pointed than it is today. Puntiagudo is also given the name Cerro Cenizas. Puntiagudo is partially contained within Vicente Pérez Rosales National Park. See also * List of volcanoes in Chile The Smithsonian Institution's Global Volcanism Program lists 105 volcanoes in Chile that have been active during the Holocene.
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Cordón Caulle
Cordón is a central ''barrio'' (neighbourhood or district) of Montevideo, Uruguay, located East of the Centro. Its main avenue is 18 de Julio Avenue. History Cordón was the first neighborhood to be created outside the walls of the old Citadel of Montevideo. In its origins it was known as "''El Cardal''", due to the fact that thistles () grew in the fields dedicated to the cultivation of corn. It was a large vacant lot that extended to the other side of the wall, behind the "''Ejidos''", that is, after the area of open land that was used for the defense of the Citadel. In 1765 the Spanish Crown ordered Bartolomé Mitre Martínez to delineate approximately 60 blocks for population. The area to the east of the demarcation was called "''Cordón''", from which the name of the neighborhood comes, because the land marking work was carried out using laces (). In January 1807 the entire area was the scene of the Battle of Cardal in the framework of the second British invasion of th ...
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Puyehue (volcano)
Puyehue (Mapudungun: ''Puye'' (small fish), ''hue'' (place)) may refer to: *Puyehue Lake *Puyehue Volcano *Puyehue National Park *Cardenal Antonio Samoré Pass formerly known as ''Puyehue Pass'' *Puyehue, Chile a commune in Osorno Province *Puyehue Hot Springs The Puyehue Hot Springs (Spanish: ''Termas de Puyehue'') is a series of hot springs located 76 kilometers along Route 215-CH east of Osorno, a city 20 kilometers from Puerto Montt in the Los Lagos Region of southern Chile. The area is served by ...
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Puyehue National Park
Puyehue National Park () is located in the Andes mountain range, in Los Ríos and Los Lagos regions of Chile formerly referred to as the 10th region. The park boast 220,000 acres of natural thermal springs, volcanoes, and evergreen forests, after having been expanded in 1950 and 1981. The park is Chile's most visited national park with 400,000 people enjoying it each year. Puyehue National park forms part of the Reserve of Temperate Rainy Forest Biospheres of the Southern Andes. Chile Route 215 passes through the park, which connects with the Argentine Route 231 via Cardenal Antonio Samoré Pass. Location The park lies in the Osorno Province, town of Puyehue. It is 118 miles northeast of Puerto Montt, or 50 miles east of Osorno. Destinations The park is dominated by Puyehue volcano, Cordón Caulle and Antillanca Group. The park is divided into three main areas: Aguas Calientes, Anticura, and Antillanca. Each area has special activities according to its landscape. Aguas Cali ...
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Puyehue Lake
Puyehue Lake (), (Mapudungun: ''puye'', "small fish" and ''hue'', "place") is an Andes, Andean Foothills, piedmont lake on the border of Los Lagos Region with Los Ríos Region of Chile. Puyehue is a lake of glacial origin. Several times during the Pleistocene glaciations, the lake depression was occupied by a large glacial lobe of the Patagonian Ice Sheet, which formed a series of moraines along its western shore. The lake has an east-west elongated shape with Fresia Island in the middle and two minor peninsulas pointing toward the island, one from the north and one from the south. The lake has a remarkably smooth shoreline, with only one inlet of significance: Futacullín Bay on the south. Entre Lagos at the western end is the only town on the lake. As with most other lakes of Zona Sur, southern Chile, Puyehue Lake acts as a sediment trap for material from the Andes. Sediment cores taken from Puyehue Lake in 2001 and 2002 have been interpreted as supporting the existence of the L ...
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