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 |
|---|---|---|---|
| 1450 ± 100 lat | — | ? | Isotopic: 14C (calibrated) |
| 910 ± 500 lat | — | ? | Isotopic: 14C (calibrated) |
| 440 ± 100 lat | — | ? | Isotopic: 14C (calibrated) |
| ok. 150 p.n.e. | — | ? | Correlation: Tephrochronology |
| 250 p.n.e. ± 200 lat | — | 4 | Isotopic: 14C (calibrated) |
| 400 p.n.e. ± 50 lat | — | ? | Correlation: Tephrochronology |
| 500 p.n.e. ± 50 lat | — | ? | Correlation: Tephrochronology |
| 610 p.n.e. ± 100 lat | — | ? | Isotopic: 14C (calibrated) |
| 650 p.n.e. ± 50 lat | — | ? | Correlation: Tephrochronology |
| 700 p.n.e. ± 50 lat | — | ? | Correlation: Tephrochronology |
| ok. 2 550 p.n.e. | — | 3 | Isotopic: 14C (uncalibrated) |
| ok. 2 750 p.n.e. | — | 2 | Isotopic: 14C (uncalibrated) |
| ok. 3 650 p.n.e. | — | 3 | Isotopic: 14C (calibrated) |
| 3 850 p.n.e. ± 200 lat | — | ? | Isotopic: 14C (calibrated) |
| ok. 4 850 p.n.e. | — | 2 | Isotopic: 14C (calibrated) |
| ok. 5 050 p.n.e. | — | 3 | Isotopic: 14C (calibrated) |
| ok. 5 350 p.n.e. | — | 3 | Isotopic: 14C (calibrated) |
| ok. 5 550 p.n.e. | — | 2 | Isotopic: 14C (calibrated) |
| 7 800 p.n.e. ± 300 lat | — | ? | Isotopic: 14C (calibrated) |
| ok. 8 050 p.n.e. | — | 3 | Isotopic: 14C (calibrated) |
Dane: Global Volcanism Program, Smithsonian Institution (#321030)