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 |
|---|---|---|---|
| 1550 ± 100 lat | — | 0 | Near South Cape · Isotopic: 14C (calibrated) |
| 1420 ± 20 lat | — | 0 | Central Taveuni (Tutu area) · Isotopic: 14C (calibrated) |
| 1350 ± 75 lat | — | 2 | Correlation: Tephrochronology |
| 1160 ± 150 lat | — | 2 | Southern Taveuni (Vana Kei Vuna) · Isotopic: 14C (calibrated) |
| ok. 1020 | — | 2 | Correlation: Tephrochronology |
| ok. 880 | — | 2 | Correlation: Tephrochronology |
| ok. 770 | — | 2 | Correlation: Tephrochronology |
| 640 ± 40 lat | — | 2 | Isotopic: 14C (calibrated) |
| 520 ± 100 lat | — | 2 | South Taveuni (Tavuyaga, Ngatutu, Ngatavo) · Isotopic: 14C (calibrated) |
| 480 ± 75 lat | — | 2 | Central Taveuni (Tagimoucea area) · Isotopic: 14C (calibrated) |
| 400 ± 50 lat | — | 2 | Isotopic: 14C (calibrated) |
| ok. 350 | — | 2 | Central Taveuni (Des Voeux Peak area) · Correlation: Tephrochronology |
| 320 ± 100 lat | — | 2 | Isotopic: 14C (calibrated) |
| ok. 270 | — | 1 | Central Taveuni (west of Lake Tagimoucea) · Correlation: Tephrochronology |
| 220 ± 100 lat | — | 0 | Isotopic: 14C (calibrated) |
| 90 p.n.e. ± 200 lat | — | 2 | Isotopic: 14C (calibrated) |
| ok. 200 p.n.e. | — | 2 | Correlation: Tephrochronology |
| 330 p.n.e. ± 75 lat | — | 2 | Isotopic: 14C (calibrated) |
| 400 p.n.e. ± 20 lat | — | 2 | Isotopic: 14C (calibrated) |
| ok. 600 p.n.e. | — | 2 | Correlation: Tephrochronology |
| ok. 680 p.n.e. | — | 2 | Correlation: Tephrochronology |
| ok. 1 020 p.n.e. | — | 2 | Correlation: Tephrochronology |
| ok. 1 100 p.n.e. | — | 2 | Correlation: Tephrochronology |
| ok. 1 200 p.n.e. | — | 2 | Correlation: Tephrochronology |
| ok. 1 300 p.n.e. | — | 2 | Correlation: Tephrochronology |
| ok. 1 450 p.n.e. | — | 2 | Correlation: Tephrochronology |
| ok. 1 700 p.n.e. | — | 2 | Correlation: Tephrochronology |
| 3 200 p.n.e. ± 150 lat | — | 2 | Isotopic: 14C (calibrated) |
| 3 580 p.n.e. ± 200 lat | — | 2 | Isotopic: 14C (calibrated) |
| 4 800 p.n.e. ± 100 lat | — | 2 | Isotopic: 14C (calibrated) |
| 5 230 p.n.e. ± 100 lat | — | 2 | Isotopic: 14C (calibrated) |
| 5 920 p.n.e. ± 75 lat | — | 2 | Isotopic: 14C (calibrated) |
| 6 560 p.n.e. ± 75 lat | — | 2 | Isotopic: 14C (calibrated) |
| 8 040 p.n.e. ± 50 lat | — | 2 | Isotopic: 14C (calibrated) |
Dane: Global Volcanism Program, Smithsonian Institution (#245010)