Lava domes are common features on volcanoes around the world. Lava domes are volcanoes 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.
the mount Ammar
| 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 |