| Puricó complex | |
|---|---|
 The southwest part of the complex is formed by the cinder cone Cerro Negro and the stratovolcano Cerros de Macón. | |
| Highest point | |
| Elevation | 5,703 m (18,711 ft)[1] |
| Coordinates | 22°57′S 67°45′W / 22.950°S 67.750°W[2] |
| Geography | |
| Location | Chile |
| Geology | |
| Age of rock | Holocene |
| Mountain type | Pyroclastic shield, volcanic complex |
The Purico complex is a Pleistocene volcanic complex in Chile close to Bolivia, formed by an ignimbrite, several lava domes and stratovolcanoes and one maar. It is in the Chilean segment of the Central Volcanic Zone, one of the four volcanic belts which make up the Andean Volcanic Belt. The Central Volcanic Zone spans Peru, Bolivia, Chile and Argentina and includes 44 active volcanoes as well as the Altiplano–Puna volcanic complex, a system of large calderas and ignimbrites of which Purico is a member. Licancabur to the north, La Pacana southeast and Guayaques to the east are separate volcanic systems.
The Purico complex consists of a shield shaped volcanic structure consisting of the Purico ignimbrite and a number of secondary volcanoes that are emplaced on this volcanic shield. During the ice ages, the shield was in part covered by glaciers which have left moraines. Purico is the source of the Purico ignimbrite, which has a volume of about 80–100 cubic kilometres (19–24 cu mi). After the emplacement of the Purico ignimbrite, a number of lava domes and stratovolcanoes developed on the ignimbrite shield. The maar of Alitar is still fumarolically active. In historical times, sulfur was mined on Purico. Today, the Llano de Chajnantor Observatory lies on the ignimbrite shield.
- ^ Cite error: The named reference
GVPwas invoked but never defined (see the help page). - ^ Francis et al. 1984, p. 106.