| Reclus | |
|---|---|
&sq=Envato&lang=en&file=File:Amalia_Glacier_Chile_2007-12-28.JPG) Amalia Glacier with Reclus behind | |
| Highest point | |
| Elevation | 1,000 m (3,300 ft)[1] |
| Coordinates | 50°57′50″S 73°35′05″W / 50.96389°S 73.58472°W[2] |
| Geography | |
 | |
| Location | Chile |
| Parent range | Andes |
| Geology | |
| Mountain type(s) | Cinder cone, composite volcano[1] |
| Last eruption | 1908 ± 1 year |
Reclus (named after Élisée Reclus; sometimes confused with Cerro Mano del Diablo southwest of Reclus), also written as Reclús, is a cinder cone and stratovolcano[1] located in the Southern Patagonian Ice Field, Chile. Part of the Austral Volcanic Zone of the Andes, its summit rises 1,000 metres (3,300 ft) above sea level and is capped by a crater about 1 kilometre (0.62 mi) wide. Close to the volcano lies the Amalia Glacier, which is actively eroding Reclus.
The volcano has been active during the late Pleistocene and Holocene. A large eruption – among the largest known in the Austral Volcanic Zone – occurred 15,260–14,373 years before present and released over 5 cubic kilometres (1.2 cu mi) of tephra. This tephra fell out over a large area of Patagonia as far as Tierra del Fuego, and disrupted the ecosystem in the region. Subsequently, further but smaller eruptions occurred during the Pleistocene and Holocene. The last historical eruption was in 1908.
The volcano is remote and monitoring began only recently. Two dams are located close to the volcano and might be impacted by future eruptions.