| Ancud Volcanic Complex Stratigraphic range: Oligocene–Miocene |
|
|---|---|
| Type | Geological formation |
| Sub-units | Heuihuen, Teguaco, Cocotue |
| Underlies | Quaternary and Neogene deposits including Lacui Formation |
| Overlies | Caleta Chonos Formation |
| Lithology | |
| Primary | Basaltic andesite |
| Other | Dacite |
| Location | |
| Region | Los Lagos Region |
| Country | Chile |
| Type section | |
| Named for | City of Ancud |
Ancud Volcanic Complex (Spanish: Complejo Volcánico de Ancud) is a volcanic complex of Oligocene and Miocene age located around Ancud with exposures in Chiloé Island, the Chilean mainland and smaller islets. Three subunits are recognized in the complex: Hueihuen, Teguaco and Cocotue. The complex is part of the mid-Tertiary coastal magmatic belt in south-central Chile.