Historia erupcji
VEI – wskaźnik eksplozywności wulkanicznej: 0 = wylew lawy, 4 = jak Eyjafjallajökull 2010, 6 = jak Pinatubo 1991, 7 = jak Tambora 1815. Skala jest logarytmiczna – każdy stopień to ok. 10 razy więcej materiału.
| Początek | Koniec | VEI | Miejsce i datowanie |
|---|---|---|---|
| luty 1785 | marzec 1786 | 2 | Upper SE flank · Observations: Reported |
| ok. 1700 | — | ? | Correlation: Tephrochronology |
| ok. 1590 | — | ? | North flank of main summit · Correlation: Tephrochronology |
| ok. 1570 | — | 4 | North flank of main summit · Correlation: Tephrochronology |
| ok. 1440 | — | ? | Correlation: Tephrochronology |
| ok. 1290 | — | 4 | Tarugo Corral lava dome (NE flank) · Correlation: Tephrochronology |
| ok. 1270 | — | ? | Correlation: Tephrochronology |
| ok. 1040 | — | 4 | Lava dome near eastern summit · Correlation: Tephrochronology |
| ok. 880 | — | ? | Correlation: Tephrochronology |
| ok. 260 | — | ? | Correlation: Tephrochronology |
| ok. 200 | — | ? | Correlation: Tephrochronology |
| ok. 170 | — | ? | Correlation: Tephrochronology |
| ok. 10 | — | ? | Correlation: Tephrochronology |
| ok. 180 p.n.e. | — | ? | Correlation: Tephrochronology |
| ok. 230 p.n.e. | — | ? | Correlation: Tephrochronology |
| ok. 260 p.n.e. | — | ? | Correlation: Tephrochronology |
| ok. 460 p.n.e. | — | ? | Correlation: Tephrochronology |
| ok. 510 p.n.e. | — | ? | Correlation: Tephrochronology |
| ok. 560 p.n.e. | — | ? | Correlation: Tephrochronology |
| ok. 1 300 p.n.e. | — | ? | Correlation: Tephrochronology |
| ok. 1 650 p.n.e. | — | ? | Correlation: Tephrochronology |
| ok. 1 800 p.n.e. | — | ? | Correlation: Tephrochronology |
Dane: Global Volcanism Program, Smithsonian Institution (#352006)