The dramatic summit spire of Volcán Corcovado is seen here in an aerial view from the south. 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. Click an entity to go directly to the entity box. For each MODIS image, the algorithm automatically scans each 1 km pixel within it to check for high-temperature hot-spots. 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. Volcanes de Chile. The most distinctive feature of this volcano is its stepped top, similar to that of Puntiagudo Volcano. 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. Darwin observed activity from the Corcovado area in 1834, and an eruption was reported to have occurred in November 1835. Locations with converging in which at least one plate is oceanic at the boundary have volcanoes. When one is found the date, time, location, and intensity are recorded. 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. The presence of a hot spot is inferred by anomalous volcanism (i.e. Before 2008, it consisted mainly of a rhyolitic lava dome last active 9,400 years ago.

Catalog of Active Volcanoes of the World and Solfatara Fields, Rome: IAVCEI, 15: 1-55. Hot spots also develop beneath continents. The light-colored delta at the left was formed by lahar deposition during the eruption of Chaitén volcano beginning in 2008. Converging plates can be oceanic, continental, or one of each.

The glacially eroded volcano is flanked by Holocene cinder cones. There is no Emissions History data available for Corcovado. Features are organized into four major categories: Cones, Craters, Domes, and Thermal Features. 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). There is no Deformation History data available for Corcovado. Make me an Ambassador. Very small-scale maps (such as world maps) are not included. The volcano seen from the west on a commercial flight. The Global Volcanism Program has no activity reports for Corcovado. The Global Volcanism Program has no Bulletin Reports available for Corcovado. C. Darwin described seing it in activity in 1834 and an explosive eruption was reported to have occurred in November 1835 by a resident from Chiloe, 60 km west of the volcano. If both are continental they will smash together and form a mountain range. If at least one is oceanic, it will subduct. Corcovado dominates the landscape of the Gulf of Corcovado area and is visible from Chiloé Island, weather permitting. 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 (?). Last eruption :     4920 BC ± 100. 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. Chilean Continent. The maps database originated over 30 years ago, but was only recently updated and connected to our main database. The volcano and the adjacent area form part of Corcovado National Park. The volcano's base has likely prehistoric lava flows that are densely vegetated.

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. Type :                     Stratovolcano Little is known about Volcán Coronado and it is unknown when it last erupted. 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. Clicking on the small images will load the full 300 dpi map. Eruptions were reported in historical time from these flank cones. Gonzalez-Ferran O, 1995. The volcano rises across the Gulf of Corcovado, which lies beyond the ridge in the middle distance. 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. 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. Subduction-zone volcanoes occur on the overriding plate and are offset inland from the actual plate boundary along the ocean trench. In some cases additional feature type, elevation, or location details are provided. comm.). The following references have all been used during the compilation of data for this volcano, it is not a comprehensive bibliography. Chaitén is a small volcanic caldera located on the flank of the Michinmahuida volcano in southern Chile. A subducting plate creates volcanoes. Do you know this place? Elevation :             2,300 m (7,546 ft) Santiago: Instituto Geografico Militar, 635 p. There is data available for 5 Holocene eruptive periods. The glacially eroded volcano is surrounded by Holocene cinder cones. Casertano L, 1963. Recreation / Outdoor near Corcovado Volcano. The main edifice at Corcovado is likely Pleistocene in age, but historical eruptions have been reported, probably from Holocene cinder cones surrounding the volcano. Corcovado, probably of late-Pleistocene age, is eroded by glaciers and surrounded by Holocene cinder cones. The IAVCEI Commission on Volcanic Hazards and Risk has a, Middle InfraRed Observation of Volcanic Activity (. Upload your photo of Corcovado Volcano! The volcano and the adjacent area form part of Corcovado National Park. 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. A series of lakes flank the eastern side of the basaltic to basaltic-andesite structure. The glacially eroded volcano is flanked by Holocene cinder cones. The glacially eroded volcano is flanked by Holocene cinder cones. Corcovado Volcano Plate Boundary; Corcovado Volcano Climb; Entity Index This is the list of all entities in this result page. This compilation of synonyms and subsidiary features may not be comprehensive. 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. At its foot lies a series of lakes. There are no samples for Corcovado in the Smithsonian's NMNH Department of Mineral Sciences Rock and Ore collection. 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. 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 is ice-covered and basaltic to basaltic-andesite in composition. Grow your travel business and get new leads from interested customers. Coronado volcano is a small stratovolcano in the Gulf of California. The most distinctive feature of this volcano is its stepped top, similar to that of Puntiagudo Volcano. 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. 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. Each day updated global maps are compiled to display the locations of all hot spots detected in the previous 24 hours. 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. The roughly 440-m-high volcano contains a 300 x 160 m wide crater. Corcovado volcano is an isolated and little studied stratovolcano in southern Chile. At its foot lies a series of beautiful lakes. Corcovado Volcano is a stratovolcano located about 25 km south of the mouth of Yelcho River, in the Palena Province, Los Lagos Region, Chile.

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