Here's the our members favorite photos of "Volcanoes in Quellon". WOVOdat is a database of volcanic unrest; instrumentally and visually recorded changes in seismicity, ground deformation, gas emission, and other parameters from their normal baselines. Corcovado, probably of late-Pleistocene age, is eroded by glaciers and surrounded by Holocene cinder cones. At its foot lies a series of beautiful lakes. Very small-scale maps (such as world maps) are not included. The glacially eroded volcano is flanked by Holocene cinder cones. Smithsonian / USGS Weekly Volcanic Activity Report, Eruptions, Earthquakes & Emissions Application, Department of Mineral Sciences Rock and Ore collection, Incorporated Research Institutions for Seismology (IRIS), World Organization of Volcano Observatories (WOVO), Large Magnitude Explosive Volcanic Eruptions (LaMEVE), Volcano Global Risk Identification and Analysis Project (VOGRIPA), Integrated Earth Data Applications (IEDA), Corcobado | Jorobado | Chiloe, Volcan de (?). At its foot lies a series of lakes. Elevation : 2,300 m (7,546 ft) The main edifice at Corcovado is likely Pleistocene in age, but historical eruptions have been reported, probably from Holocene cinder cones surrounding the volcano. Little is known of this isolated volcano that was seen in eruption by Darwin in 1834, and an eruption was reported to have occurred in November 1835. Last eruption : 4920 BC ± 100. Volcanes de Chile. There is no Emissions History data available for Corcovado. This compilation of synonyms and subsidiary features may not be comprehensive. The most distinctive feature of this volcano is its stepped top, similar to that of Puntiagudo Volcano. Corcovado dominates the landscape of the Gulf of Corcovado area and is visible from Chiloé Island, weather permitting. The light-colored delta at the left was formed by lahar deposition during the eruption of Chaitén volcano beginning in 2008. © TouristLink.com 2020, All Rights Reserved. Corcovado Volcano is a stratovolcano located about 25 km south of the mouth of Yelcho River, in the Palena Province, Los Lagos Region, Chile. Although the process is not clearly understood, magma apparently forms and rises by buoyancy from a depth of 100 to 200 km (60 to 120 miles). The glacially eroded volcano is flanked by Holocene cinder cones. Clicking on the small images will load the full 300 dpi map. Upload your photo of Corcovado Volcano! The most distinctive feature of this volcano is its stepped top, similar to that of Puntiagudo Volcano. The presence of a hot spot is inferred by anomalous volcanism (i.e. The maps shown below have been scanned from the GVP map archives and include the volcano on this page. The Hawaiian hot spot has been active at least 70 million years, producing a volcanic chain that extends 3,750 miles (6,000 km) across the northwest Pacific Ocean. Hot spots also develop beneath continents. In some cases additional feature type, elevation, or location details are provided. The volcano rises across the Gulf of Corcovado, which lies beyond the ridge in the middle distance. Corcovado Volcano Plate Boundary; Corcovado Volcano Climb; Entity Index This is the list of all entities in this result page. Two of a string of lakes on its eastern side appear in the background. There is a drop-down list with volcano names which allow users to 'zoom-in' and examine the distribution of hot-spots at a variety of spatial scales. Using infrared satellite Moderate Resolution Imaging Spectroradiometer (MODIS) data, scientists at the Hawai'i Institute of Geophysics and Planetology, University of Hawai'i, developed an automated system called MODVOLC to map thermal hot-spots in near real time. The most distinctive feature of this volcano is its stepped top, similar to that of Puntiagudo Volcano. Subduction-zone volcanoes occur on the overriding plate and are offset inland from the actual plate boundary along the ocean trench. Corcovado Volcano is a stratovolcano located about 25 km south of the mouth of Yelcho River, in the Palena Province, Los Lagos Region, Chile. Corcovado is ice-covered and basaltic to basaltic-andesite in composition. It is sponsored by the, Information about large Quaternary eruptions (VEI >= 4) is cataloged in the, EarthChem develops and maintains databases, software, and services that support the preservation, discovery, access and analysis of geochemical data, and facilitate their integration with the broad array of other available earth science parameters. The IAVCEI Commission on Volcanic Hazards and Risk has a, Middle InfraRed Observation of Volcanic Activity (. The volcano seen from the west on a commercial flight. Note: volcanoes are ordered by latitude from north to south, 180 Degrees South: Conquerors of the Useless, "Holocene tephrochronology of the southernmost part (42°30'-45°S) of the Andean Southern Volcanic Zone", https://en.wikipedia.org/w/index.php?title=Corcovado_Volcano&oldid=969649742, Creative Commons Attribution-ShareAlike License, This page was last edited on 26 July 2020, at 17:56. Do you know this place? Gonzalez-Ferran O, 1995. When one is found the date, time, location, and intensity are recorded. Corcovado dominates the landscape of Gulf of Corcovado area and is visible from the Chiloé Island, weather allowing. Converging plates can be oceanic, continental, or one of each. Santiago: Instituto Geografico Militar, 635 p. There is data available for 5 Holocene eruptive periods. Its only known historic activity was in 1834 and/or 1835. There is no Deformation History data available for Corcovado. Features are organized into four major categories: Cones, Craters, Domes, and Thermal Features. If at least one is oceanic, it will subduct. Darwin observed activity from the Corcovado area in 1834, and an eruption was reported to have occurred in November 1835. Corcovado, probably of late-Pleistocene age, is eroded by glaciers and surrounded by Holocene cinder cones. Locations with converging in which at least one plate is oceanic at the boundary have volcanoes. The town of Chaitén was formerly the main gateway to this protected area. The dramatic summit spire of Corcovado volcano is seen in this telephoto view from the west from the town of Quellon on the island of Chiloe. Corcovado Volcano (Spanish pronunciation: [koɾkoˈβaðo]) is a stratovolcano located about 25 kilometres (16 mi) south of the mouth of the Yelcho River, in the Palena Province, Los Lagos Region, Chile. The Global Volcanism Program has no Bulletin Reports available for Corcovado. We welcome users to tell us if they see incorrect information or other problems with the maps; please use the Contact GVP link at the bottom of the page to send us email. Chaitén is a small volcanic caldera located on the flank of the Michinmahuida volcano in southern Chile. Little is known about Volcán Coronado and it is unknown when it last erupted. Recreation / Outdoor near Corcovado Volcano. The volcano's base has likely prehistoric lava flows that are densely vegetated. The glacially eroded volcano is flanked by Holocene cinder cones. The Global Volcanism Program has no activity reports for Corcovado. Make me an Ambassador. It forms a 2 km wide peninsula at the northern tip of Coronado Island, 3 km off the eastern coast of Baja California in the Canal de los Ballenas. At its foot lies a series of beautiful lakes. The dramatic summit spire of Volcán Corcovado is seen here in an aerial view from the south. If both are continental they will smash together and form a mountain range. The sharp-topped peak of Corcovado volcano rises above the Gulf of Corcovado as seen from the north from a helicopter near the town of Chaitén. not at a plate boundary), such as the Hawaiian volcanoes within the Pacific Plate. The roughly 440-m-high volcano contains a 300 x 160 m wide crater. The volcano and the adjacent area form part of Corcovado National Park. The town of Chaitén was formerly the main gateway to this protected area, but much of the town was destroyed by an eruption of Chaitén Volcano and the resultant mudflow in 2008. A series of lakes flank the eastern side of the basaltic to basaltic-andesite structure. There are no samples for Corcovado in the Smithsonian's NMNH Department of Mineral Sciences Rock and Ore collection. Click an entity to go directly to the entity box. Synonyms of features appear indented below the primary name. Eruptions were reported in historical time from these flank cones. Type : Stratovolcano The eruption has had serious consequences for the nearby town of Chaitén… Corcovado Volcano (Spanish pronunciation: [koɾkoˈβaðo]) is a stratovolcano located about 25 kilometres (16 mi) south of the mouth of the Yelcho River, in the Palena Province, Los Lagos Region, Chile. Corcovado has had two unconfirmed eruptions in 1834 and 1835 with lava flows from flank cones, which are probably based on confusion with Michinmahuida volcano. Three tephra layers are linked to Corcovado volcano, of which the two youngest are dated 7,980 BP and 6,870 BP respectively. The volcano rises across the Gulf of Corcovado, which lies beyond the ridge in the middle distance. The Global Volcanism Program has no Weekly Reports available for Corcovado. Coronado volcano is a small stratovolcano in the Gulf of California. The glacially eroded volcano is surrounded by Holocene cinder cones. The following references have all been used during the compilation of data for this volcano, it is not a comprehensive bibliography. Corcovado Volcano Stratovolcano in Chile; 180° South 2010 film; Wiki Authority Control Authority control is a method of creating and maintaining index terms for bibliographical material in a library catalogue. A subducting plate creates volcanoes. Catalog of Active Volcanoes of the World and Solfatara Fields, Rome: IAVCEI, 15: 1-55. EarthChem is operated by a joint team of disciplinary scientists, data scientists, data managers and information technology developers who are part of the NSF-funded data facility. Chilean Continent. For each MODIS image, the algorithm automatically scans each 1 km pixel within it to check for high-temperature hot-spots. Eruptions in historical time were considered likely from these postglacial volcanoes (Moreno 1985, pers. Photo by Bryan Freeman, 2005. The main edifice at Corcovado is likely Pleistocene in age, but historical eruptions have been reported, probably from Holocene cinder cones surrounding the volcano. But in May 2008, Chaitén began erupting violently, producing numerous plumes, pyroclastic flows and lahars, and building a new lava dome on the north side of the old one. Before 2008, it consisted mainly of a rhyolitic lava dome last active 9,400 years ago. 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