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 |
|---|---|---|---|
| 15 sierpnia 1999 | trwa | 4 | Observations: Reported |
| 3 kwietnia 1999 | 12 kwietnia 1999 | 2 | Observations: Reported |
| 30 maja 1998 | 3 września 1998 | 3 | Observations: Reported |
| 8 marca 1997 | 4 kwietnia 1997 | 2 | Observations: Reported |
| 10 stycznia 1990 | 16 lutego 1995 | 3 | Observations: Reported |
| 7 kwietnia 1989 | 26 czerwca 1989 | 2 | Observations: Reported |
| 7 grudnia 1988 | 7 grudnia 1988 | 2 | Observations: Reported |
| 28 marca 1986 | 28 lutego 1988 | 3 | Observations: Reported |
| 26 maja 1985 | 25 października 1985 | 2 | Observations: Reported |
| 17 marca 1984 | 6 września 1984 | 2 | Observations: Reported |
| 23 sierpnia 1980 | 1 grudnia 1981 | 1 | Center of 1964 crater · Observations: Reported |
| 12 listopada 1964 | 12 listopada 1964 | 4 | Molodoy Sheveluch summit domes · Observations: Reported |
| 5 listopada 1944 | 6 kwietnia 1950 | 2 | Suelich · Observations: Reported |
| 1 lutego 1930 | — | 1 | Observations: Reported |
| 27 stycznia 1928 | 15 kwietnia 1929 | 1 | Observations: Reported |
| 2 lipca 1905 | — | ? | Observations: Reported |
| 2 lipca 1897 | 2 lipca 1898 | 2 | Observations: Reported |
| 2 lipca 1879 | 2 lipca 1883 | 3 | Observations: Reported |
| 18 lutego 1854 | — | 5 | Observations: Reported |
| 1739 | — | 3 | Observations: Reported |
| ok. 1700 | — | 3 | Correlation: Tephrochronology |
| 1652 ± 11 lat | — | 5 | Isotopic: 14C (calibrated) |
| ok. 1550 | — | 3 | Correlation: Tephrochronology |
| ok. 1430 | — | 4 | Isotopic: 14C (calibrated) |
| ok. 1150 | — | 3 | Correlation: Tephrochronology |
| 1034 ± 23 lata | — | 5 | Isotopic: 14C (calibrated) |
| ok. 1020 ± 40 lat | — | 3 | Correlation: Tephrochronology |
| ok. 970 ± 80 lat | — | 4 | Isotopic: 14C (calibrated) |
| ok. 750 | — | 3 | Correlation: Tephrochronology |
| ok. 700 | — | 3 | Correlation: Tephrochronology |
| 650 ± 40 lat | — | 5 | Isotopic: 14C (calibrated) |
| ok. 630 | — | 3 | Western flank (Karan) · Correlation: Tephrochronology |
| ok. 600 | — | 5 | Isotopic: 14C (calibrated) |
| ok. 580 | — | 4 | Correlation: Tephrochronology |
| ok. 530 | — | 3 | Correlation: Tephrochronology |
| ok. 500 | — | 4 | Isotopic: 14C (calibrated) |
| ok. 380 | — | 3 | Isotopic: 14C (calibrated) |
| ok. 250 | — | 4 | Correlation: Tephrochronology |
| ok. 230 | — | 3 | Correlation: Tephrochronology |
| 170 ± 20 lat | — | 3 | Isotopic: 14C (calibrated) |
| ok. 120 | — | 3 | Isotopic: 14C (calibrated) |
| ok. 100 | — | 4 | Correlation: Tephrochronology |
| ok. 10 p.n.e. | — | 3 | Correlation: Tephrochronology |
| ok. 150 p.n.e. | — | 3 | West flank (Karan) · Correlation: Tephrochronology |
| ok. 300 p.n.e. | — | 4 | West flank (Karan) · Isotopic: 14C (calibrated) |
| ok. 400 p.n.e. | — | 3 | West flank (Karan) · Correlation: Tephrochronology |
| ok. 500 p.n.e. | — | 4 | Isotopic: 14C (calibrated) |
| ok. 650 p.n.e. | — | 3 | Correlation: Tephrochronology |
| 780 p.n.e. ± 300 lat | — | 4 | Isotopic: 14C (calibrated) |
| ok. 900 p.n.e. | — | 3 | Correlation: Tephrochronology |
| ok. 950 p.n.e. | — | 5 | Isotopic: 14C (calibrated) |
| ok. 1 010 p.n.e. | — | 3 | Correlation: Tephrochronology |
| 1 330 p.n.e. ± 200 lat | — | 3 | Isotopic: 14C (calibrated) |
| ok. 1 500 p.n.e. | — | 3 | Correlation: Tephrochronology |
| ok. 1 650 p.n.e. | — | 3 | Correlation: Tephrochronology |
| ok. 1 700 p.n.e. | — | 4 | Correlation: Tephrochronology |
| ok. 2 000 p.n.e. | — | 5 | Isotopic: 14C (calibrated) |
| ok. 2 100 p.n.e. | — | 5 | Isotopic: 14C (calibrated) |
| ok. 2 150 p.n.e. | — | 3 | Correlation: Tephrochronology |
| ok. 2 200 p.n.e. | — | 4 | Correlation: Tephrochronology |
| ok. 2 490 p.n.e. | — | 3 | Isotopic: 14C (calibrated) |
| ok. 2 530 p.n.e. | — | 3 | Correlation: Tephrochronology |
| 2 620 p.n.e. ± 300 lat | — | 5 | Isotopic: 14C (calibrated) |
| ok. 2 750 p.n.e. | — | 3 | Correlation: Tephrochronology |
| ok. 2 900 p.n.e. | — | 3 | Correlation: Tephrochronology |
| ok. 3 050 p.n.e. | — | 3 | Correlation: Tephrochronology |
| ok. 3 200 p.n.e. | — | 4 | Correlation: Tephrochronology |
| ok. 3 500 p.n.e. | — | 5 | Isotopic: 14C (calibrated) |
| ok. 3 650 p.n.e. | — | 5 | Isotopic: 14C (calibrated) |
| ok. 4 250 p.n.e. | — | 3 | Correlation: Tephrochronology |
| ok. 4 350 p.n.e. | — | 3 | Isotopic: 14C (calibrated) |
| ok. 4 400 p.n.e. | — | 5 | Isotopic: 14C (calibrated) |
| ok. 4 530 p.n.e. | — | 3 | Isotopic: 14C (calibrated) |
| ok. 4 900 p.n.e. | — | 3 | Correlation: Tephrochronology |
| ok. 5 400 p.n.e. | — | 3 | Correlation: Tephrochronology |
| ok. 5 500 p.n.e. | — | 5 | Correlation: Tephrochronology |
| ok. 6 000 p.n.e. | — | 3 | Correlation: Tephrochronology |
| ok. 6 100 p.n.e. | — | 3 | Correlation: Tephrochronology |
| ok. 6 200 p.n.e. | — | 3 | Correlation: Tephrochronology |
| ok. 6 350 p.n.e. | — | 4 | Correlation: Tephrochronology |
| ok. 6 380 p.n.e. | — | 4 | Correlation: Tephrochronology |
| 6 400 p.n.e. ± 150 lat | — | 4 | Isotopic: 14C (calibrated) |
| ok. 6 500 p.n.e. | — | 3 | Correlation: Tephrochronology |
| ok. 6 600 p.n.e. | — | 4 | Correlation: Tephrochronology |
| ok. 6 800 p.n.e. | — | 5 | Correlation: Tephrochronology |
| ok. 7 000 p.n.e. | — | 3 | Correlation: Tephrochronology |
| ok. 7 150 p.n.e. | — | 5 | Correlation: Tephrochronology |
| ok. 7 300 p.n.e. | — | 5 | Correlation: Tephrochronology |
| 7 400 p.n.e. ± 150 lat | — | 5 | Isotopic: 14C (calibrated) |
| ok. 7 500 p.n.e. | — | 4 | Correlation: Tephrochronology |
| ok. 7 550 p.n.e. | — | 3 | Correlation: Tephrochronology |
| ok. 7 600 p.n.e. | — | 4 | Correlation: Tephrochronology |
| ok. 7 630 p.n.e. | — | 4 | Correlation: Tephrochronology |
| ok. 7 700 p.n.e. | — | 4 | Correlation: Tephrochronology |
| ok. 7 750 p.n.e. | — | 3 | Correlation: Tephrochronology |
| ok. 7 850 p.n.e. | — | 3 | Correlation: Tephrochronology |
| ok. 7 950 p.n.e. | — | 4 | Correlation: Tephrochronology |
| ok. 8 100 p.n.e. | — | 4 | Correlation: Tephrochronology |
| ok. 8 200 p.n.e. | — | 4 | Correlation: Tephrochronology |
| ok. 8 350 p.n.e. | — | 4 | Correlation: Tephrochronology |
| ok. 8 450 p.n.e. | — | 3 | Correlation: Tephrochronology |
| ok. 8 500 p.n.e. | — | 3 | Correlation: Tephrochronology |
Dane: Global Volcanism Program, Smithsonian Institution (#300270)