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Mocho-Choshuenco
Mocho-Choshuenco (Pronounced: ) is a glacier covered compound stratovolcano in the Andes of Los Ríos Region, Chile. It is made of the twin volcanoes Choshuenco in the northwest and the Mocho in the southeast. The highest parts of the volcano are part of the Mocho-Choshuenco National Reserve while the eastern slopes are partly inside the Huilo-Huilo Natural Reserve. Choshuenco, located on the northwest rim of the 4 km wide caldera, is of late glacial age. It has a heavily eroded crater and is currently dormant. Mocho is an andesitic-dacitic volcano placed above the caldera. Some parasitic craters and cinder cones are located on the southwest and northeast flanks of the stratovolcano. Mocho has its earliest certainly recorded eruption in 1759, older eruptions reported are uncertain due to the usage of different names and inexact maps. The northern foothills of Mocho-Choshuenco are surrounded by an arc of rivers and lakes formed by Fui, Enco and Llanquihue River, and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mocho-Choshuenco National Reserve
The Mocho-Choshuenco National Reserve (Pronounced: ) is a natural reserve around the Mocho-Choshuenco volcano, in Los Ríos Region, southern Chile. The reserve was created by decree in March 1994 and covers distributed in Panguipulli, Los Lagos and Futrono municipality. The principal access goes from the Pan American Highway to Enco passing by Panguipulli and Choshuenco. From Enco a small way goes to the refuge area, during the summer months tracked vehicles can go there. Mocho-Choshuenco National Reserve has no park guards or any public infrastructure. In the refuge sector there is a mountain hut leased to Los Lagos municipality, some old military buildings ruins, and the rests of a small ski centre. Gallery image:Riñihue.jpg, Sunset on Riñihue Lake, view from Mocho-Choshuenco File:Rioblanco 1608515578.jpg, Río Blanco Valley. Río Blanco river drains the west side of Mocho-Choshuenco to the Enco River The Enco River (Spanish: ''Río Enco'') is a river in Panguipulli ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Huilo-Huilo Natural Reserve
Huilo-Huilo Biological Reserve ( , Pronounced: ) is a private for profit natural reserve and ecotourism area in southern Chile. It is by the community of Neltume along the international road to Hua Hum Pass near the border to Argentina. The reserve has unique hotels, including Montana Mágica, the Nothofagus hotel, cabins, and a lodge for backpackers. The grounds also include a brewery, various animal habitats, a funicular, and many miles of trails. The reserve includes many waterfalls and the eastern slopes of Mocho-Choshuenco, a glacial compound stratovolcano. History In the 1960 and 1970s, prior to the creation of the reserve, the area had a strong lumberjack-campesino labour movement. It was for this reason that Revolutionary Left Movement chose it to create a focus of resistance inspired by the Fidel Castro's 26th of July Movement in the Sierra Maestra in order to combat Pinochet's dictatorship. The Chilean army succeeded in isolating the group by August 1981 and in O ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Huilo-Huilo Falls
Huilo-Huilo Biological Reserve ( , Pronounced: ) is a private for profit natural reserve and ecotourism area in southern Chile. It is by the community of Neltume along the international road to Hua Hum Pass near the border to Argentina. The reserve has unique hotels, including Montana Mágica, the Nothofagus hotel, cabins, and a lodge for backpackers. The grounds also include a brewery, various animal habitats, a funicular, and many miles of trails. The reserve includes many waterfalls and the eastern slopes of Mocho-Choshuenco, a glacial compound stratovolcano. History In the 1960 and 1970s, prior to the creation of the reserve, the area had a strong lumberjack-campesino labour movement. It was for this reason that Revolutionary Left Movement chose it to create a focus of resistance inspired by the Fidel Castro's 26th of July Movement in the Sierra Maestra in order to combat Pinochet's dictatorship. The Chilean army succeeded in isolating the group by August 1981 and in O ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pillanleufú River
Pillanleufú River ( Mapudungun for ''river of the pillán'') is a river in Futrono, southern Chile. It drains waters from the southern and eastern slopes of Mocho-Choshuenco volcano to Maihue Lake, which in turn flows by Calcurrupe River into Ranco Lake. The river flows in a north-south direction along the Liquiñe-Ofqui Fault The Liquiñe-Ofqui Fault is major geological fault that runs a length of roughly in a NNE-SSW orientation and exhibits current seismicity. It is located in the Chilean Northern Patagonian Andes. It is a dextral intra-arc strike-slip fault. Most .... See also * List of rivers of Chile Rivers of Chile Rivers of Los Ríos Region Mapuche language {{Chile-river-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Riñihue Lake
The Riñihue Lake ( es, Lago Riñihue ) is a lake of glacial origin in eastern Valdivia Province, southern Chile. It is surrounded by several mountains. The eastern side receives the waters of the Panguipulli Lake by the Enco River, its main contributor. It is the last of the Seven Lakes chain. In the west it is cut into two arms by the Tralcán Mount, and on the east side lies the Mocho-Choshuenco volcano. In the south the lake is bounded by the Cerros de Quimán mountains. The lake's name derives from the Mapuche words ''rëngi'', "cane", and ''hue'', "place". In the 16th century the lake was known as Comohue, from ''co mu'', "with water", and ''hue'', "place". The Riñihuazo The Riñihue lake became famous after an event known as the "Riñihuazo", which threatened to destroy several towns, villages and cities in southern Chile. During the Great Chilean earthquake a landslide near the Tralcan Mount dammed the Riñihue Lake. As the water levels of Riñihue rose more than ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Panguipulli, Chile
Panguipulli ( ; Mapudungun for "hill of the puma") is a city and commune in Valdivia Province, southern Chile, administered by the Municipality of Panguipulli. It is located on the western edge of Panguipulli Lake, and is on a moraine in the Chilean Central Valley. Most of the commune lies on Andean mountains and valleys. History Panguipulli's first recorded inhabitants were indigenous Mapuches that lived along the shores of the main lakes and rivers of the region. The first mention of Panguipulli was in 1776. Guillermo Angermaier, who settled in the western shores of Panguipulli Lake in 1885, was the first non-indigenous person to settle in what is now the commune of Panguipulli. It was not until 1946 that the city was officially founded. In 1903 the Capuchin order established a mission in Panguipulli. The Capuchin monks built the first schools in the area. In 1947 the Capuchin built Panguipulli's twin towered wooden church, which is now a local landmark. 2020s Demo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Enco River
The Enco River (Spanish: ''Río Enco'') is a river in Panguipulli commune in southern Chile. Flowing from Panguipulli Lake to Riñihue Lake, it carries the water of the six upper lakes of the Seven Lakes area into Riñihue, the last lake in the chain. Located between the piedmont of Mocho-Choshuenco Volcano and Cerro Maltusado Enco River is unusual because it drains Panguipulli Lake through its eastern and mountainous end rather than allowing the lake to drain through the low moraine hills in the west. The Enco flows for nearly eight miles from Panguipulli Lake to Riñihue Lake. This course of the river is made spectacular by the presence, in the east, of the magnificent volcano Volcan Mocho. This combination of scenic landscape, clear water and considerably safe waters have made the Enco a magnet for rafters and other white water aficionados. The river has strong currents and no traffic. See also *List of rivers of Chile This list of rivers of Chile includes all the major ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Choshuenco
Choshuenco is a village ( es, aldea) on the eastern edge of Panguipulli Lake in Panguipulli commune, Los Lagos Region, Chile. It is south of the 203-CH route that goes from Lanco to Huahum Pass. It is west of the Argentina Argentina (), officially the Argentine Republic ( es, link=no, República Argentina), is a country in the southern half of South America. Argentina covers an area of , making it the List of South American countries by area, second-largest ... border. Choshuenco is served by Molco Airport. Populated places in Valdivia Province Populated lakeshore places in Chile {{LosRíos-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Puerto Fui
Puerto Fuy is a Chilean village (Spanish: ''aldea'') in Panguipulli commune, of Los Ríos Region. Puerto Fuy lies along the 203-CH route to Huahum Pass into Argentina at western edge of Pirihueico Lake and is a terminal station of the ferry A ferry is a ship, watercraft or amphibious vehicle used to carry passengers, and sometimes vehicles and cargo, across a body of water. A passenger ferry with many stops, such as in Venice, Italy, is sometimes called a water bus or water ta ... that crosses the lake connecting to Puerto Pirihueico. Populated places in Valdivia Province Populated lakeshore places in Chile {{LosRíos-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
South Volcanic Zone
The Andean Volcanic Belt is a major volcanic belt along the Andean cordillera in Argentina, Bolivia, Chile, Colombia, Ecuador, and Peru. It is formed as a result of subduction of the Nazca Plate and Antarctic Plate underneath the South American Plate. The belt is subdivided into four main volcanic zones which are separated by volcanic gaps. The volcanoes of the belt are diverse in terms of activity style, products, and morphology. While some differences can be explained by which volcanic zone a volcano belongs to, there are significant differences within volcanic zones and even between neighboring volcanoes. Despite being a type location for calc-alkalic and subduction volcanism, the Andean Volcanic Belt has a broad range of volcano-tectonic settings, as it has rift systems and extensional zones, transpressional faults, subduction of mid-ocean ridges and seamount chains as well as a large range of crustal thicknesses and magma ascent paths and different amounts of crustal assimi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Andesitic
Andesite () is a volcanic rock of intermediate composition. In a general sense, it is the intermediate type between silica-poor basalt and silica-rich rhyolite. It is fine-grained (aphanitic) to porphyritic in texture, and is composed predominantly of sodium-rich plagioclase plus pyroxene or hornblende. Andesite is the extrusive equivalent of plutonic diorite. Characteristic of subduction zones, andesite represents the dominant rock type in island arcs. The average composition of the continental crust is andesitic. Along with basalts, andesites are a component of the Martian crust. The name ''andesite'' is derived from the Andes mountain range, where this rock type is found in abundance. It was first applied by Christian Leopold von Buch in 1826. Description Andesite is an aphanitic (fine-grained) igneous rock that is intermediate in its content of silica and low in alkali metals. It has less than 20% quartz and 10% feldspathoid by volume, with at least 65% of the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Aquifer
An aquifer is an underground layer of water-bearing, permeable rock, rock fractures, or unconsolidated materials ( gravel, sand, or silt). Groundwater from aquifers can be extracted using a water well. Aquifers vary greatly in their characteristics. The study of water flow in aquifers and the characterization of aquifers is called hydrogeology. Related terms include aquitard, which is a bed of low permeability along an aquifer, and aquiclude (or ''aquifuge''), which is a solid, impermeable area underlying or overlying an aquifer, the pressure of which could create a confined aquifer. The classification of aquifers is as follows: Saturated versus unsaturated; aquifers versus aquitards; confined versus unconfined; isotropic versus anisotropic; porous, karst, or fractured; transboundary aquifer. Challenges for using groundwater include: overdrafting (extracting groundwater beyond the equilibrium yield of the aquifer), groundwater-related subsidence of land, groundwater becoming ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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