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 |
|---|---|---|---|
| ok. 2 lipca 1800 | — | ? | Correlation: Tephrochronology |
| ok. 1755 | — | ? | Sidereal: Dendrochronology |
| 1700 ± 50 lat | — | ? | Isotopic: 14C (uncalibrated) |
| ok. 1655 | — | 4 | Sidereal: Dendrochronology |
| 1590 ± 40 lat | — | ? | Isotopic: 14C (uncalibrated) |
| 1570 ± 40 lat | — | ? | Isotopic: 14C (uncalibrated) |
| 1560 ± 40 lat | — | ? | Isotopic: 14C (uncalibrated) |
| 1550 ± 40 lat | — | ? | Isotopic: 14C (uncalibrated) |
| 1500 ± 30 lat | — | ? | Isotopic: 14C (uncalibrated) |
| 1480 ± 50 lat | — | ? | Isotopic: 14C (uncalibrated) |
| 1400 ± 50 lat | — | ? | Isotopic: 14C (uncalibrated) |
| 1340 ± 40 lat | — | ? | Isotopic: 14C (uncalibrated) |
| 1300 ± 50 lat | — | ? | Isotopic: 14C (uncalibrated) |
| 1070 ± 40 lat | — | ? | Isotopic: 14C (uncalibrated) |
| 970 ± 30 lat | — | ? | Isotopic: 14C (uncalibrated) |
| 820 ± 30 lat | — | ? | Isotopic: 14C (uncalibrated) |
| ok. 550 | — | ? | Correlation: Tephrochronology |
| 520 ± 150 lat | — | ? | Isotopic: 14C (uncalibrated) |
| 390 ± 40 lat | — | ? | Isotopic: 14C (uncalibrated) |
| ok. 150 | — | 3 | Correlation: Tephrochronology |
| 100 ± 40 lat | — | ? | Isotopic: 14C (uncalibrated) |
| 40 p.n.e. ± 75 lat | — | ? | Isotopic: 14C (uncalibrated) |
| 150 p.n.e. ± 30 lat | — | ? | Isotopic: 14C (uncalibrated) |
| 420 p.n.e. ± 30 lat | — | ? | Isotopic: 14C (uncalibrated) |
| 590 p.n.e. ± 500 lat | — | ? | Correlation: Tephrochronology |
| 1 130 p.n.e. ± 200 lat | — | ? | Fanthams Peak · Correlation: Tephrochronology |
| 1 190 p.n.e. ± 40 lat | — | ? | Isotopic: 14C (uncalibrated) |
| ok. 1 250 p.n.e. | — | ? | Southern Beehive · Correlation: Tephrochronology |
| 1 560 p.n.e. ± 40 lat | — | ? | Isotopic: 14C (uncalibrated) |
| 1 700 p.n.e. ± 100 lat | — | 5 | Isotopic: 14C (uncalibrated) |
| ok. 2 150 p.n.e. | — | ? | Correlation: Tephrochronology |
| 2 400 p.n.e. ± 40 lat | — | ? | Isotopic: 14C (uncalibrated) |
| 2 450 p.n.e. ± 300 lat | — | ? | Correlation: Tephrochronology |
| ok. 2 700 p.n.e. | — | ? | Correlation: Tephrochronology |
| 2 850 p.n.e. ± 300 lat | — | ? | Correlation: Tephrochronology |
| ok. 3 250 p.n.e. | — | ? | Correlation: Tephrochronology |
| 5 120 p.n.e. ± 50 lat | — | ? | Isotopic: 14C (uncalibrated) |
| ok. 6 050 p.n.e. | — | ? | Correlation: Tephrochronology |
| 7 000 p.n.e. ± 100 lat | — | ? | Isotopic: 14C (uncalibrated) |
| 7 270 p.n.e. ± 50 lat | — | ? | Isotopic: 14C (uncalibrated) |
| ok. 7 330 p.n.e. | — | ? | Correlation: Tephrochronology |
| ok. 7 650 p.n.e. | — | ? | Isotopic: 14C (uncalibrated) |
Dane: Global Volcanism Program, Smithsonian Institution (#241030)