Lava domes are common features on volcanoes around the world. Lava domes are known to exist on plate margins as well as in intra-arc hotspots, and on heights above 6000 m and in the sea floor.[1] Individual lava domes and volcanoes featuring lava domes are listed below.
Dome or volcano name | Volcanic area | Composition | Last dome eruption or growth episode |
---|---|---|---|
Dacht-i-Navar Group | Ghanzi region | ||
Vakak Group | Ghanzi region |
Dome or volcano name | Volcanic area | Composition | Last dome eruption or growth episode |
---|---|---|---|
Tipas | Central Volcanic Zone | ||
Trocon | Southern Volcanic Zone | Andesite to Dacite |
Dome or volcano name | Volcanic area | Composition | Last dome eruption or growth episode |
---|---|---|---|
Cerros de Saltar | Central Volcanic Zone | Dacite | Pliocene |
Chaitén | Southern Volcanic Zone | Rhyolite | 2010 |
Cerro Chao | Central Volcanic Zone | Dacite | Quaternary |
Cerro Porquesa | Central Volcanic Zone | Rhyodacite | Pliocene/Pleistocene |
Chillahuita | Central Volcanic Zone | ||
Corona Dome Complex | Central Volcanic Zone | Andesite | Quaternary |
Cordón Caulle | Southern Volcanic Zone | Rhyodacite to Rhyolite | Holocene |
Fueguino | Austral Volcanic Zone | Holocene | |
Lascar | Central Volcanic Zone | Dacite | 2007 |
Volcán Nuevo | Southern Volcanic Zone | Dacite | 1986 |
Sollipulli | Southern Volcanic Zone | Andesite to Dacite | |
Taapaca | Central Volcanic Zone | Holocene |