Table 3.
Volcano | Explosive Phase selected | P1 SiO2 content (wt%) | Coding | P2 Inclusion Depth (km) | H2O (wt%) | Coding | P3Open/Closed conduit | Coding | P4Phreato-magmatism | Coding | P5Co-PDC plumes | Coding |
---|---|---|---|---|---|---|---|---|---|---|---|---|
Pinatubo | Climactic phase on 15–16/06/1991 | 78(49) | 1 | 8.5 | 6.5(49,50) | 1 | Closed(51) | 0 | No(52) | 0 | Yes(53) | 1 |
Kelut | Full eruption 13/02/2014 | 56(5) | 1 | 19 | 4.72(54) | 0 | Closed(55) | 0 | No(55) | 0 | Yes(56) | 1 |
El Chichon (events B & C) | Phases B and C on 04/04/1982 | 55.9(57) | 1 | 8 | 4(58) | 1 | Closed(59) | 0 | Yes(59) | 1 | Yes(59) | 1 |
Hudson | Full eruption 12–15/08/1991 | 60–65(60) | 1 | 4 | 3(60) | 1 | Closed(10) | 0 | Yes(61) | 1 | No(10) | 0 |
Sarychev Peak | Subplinian events on 14–15/06/2009 | 54.4(12) | 0 | 3.5 | 4(12) | 1 | Closed(12) | 0 | No(12) | 0 | Yes(12) | 1 |
Cordón Caulle | Climactic phase on 4–5/06/2011 | 67–70(62) | 1 | 3.75 | 2.7(PC) | 1 | Closed(63) | 0 | No(63) | 0 | Yes(64) | 1 |
Grimsvotn | Subplinian phase on 22/05/2011 | 50(65,66) | 0 | 15 | 0.7(66) | 0 | Closed(66) | 0 | Yes(67) | 1 | No(66) | 0 |
Mt. Spurr (1) | Full eruption 16/09/1992 | 57(68) | 1 | Closed(69) | 0 | No(70) | 0 | No(71) | 0 | |||
Mt. Spurr (2) | Full eruption 18/08/1992 | 57(68) | 1 | Closed(69) | 0 | No(70) | 0 | No(71) | 0 | |||
Redoubt (events 1 to 5) | Explosive events 1 to 5 on 22–23/03/2009 | 57–62(72) | 1 | 5 | 4.9(73) | 1 | Open(22) | 1 | No(22) | 0 | No(22) | 0 |
Mt. Spurr (3) | Full eruption 27/06/1992 | 57(68) | 1 | Closed(69) | 0 | No(70) | 0 | No(71) | 0 | |||
Lascar | Full eruption 04/1993 | 57–61(74) | 1 | 4.5 | 5(75) | 1 | Open(74) | 1 | No(74) | 0 | Yes(76) | 1 |
Anatahan | Explosive phases on 10–11/05/2003 | 60–61(77) | 1 | 1 | 3.4(78) | 1 | Closed(78) | 0 | Yes(78) | 1 | No(79) | 0 |
Chaiten | Full eruption: 2–8/05/2008 | 76(80) | 1 | 5 | 2.3(80) | 0 | Closed(80) | 0 | No(80) | 0 | No(28) | 0 |
Hekla | Phase I + 8 hrs phase II on 26/02/2000 | 55.5(81) | 0 | 9 | 2.5(82) | 0 | Closed(81) | 0 | Yes(29) | 1 | Yes(81) | 1 |
Soufrière Hills | Full eruption: 26/09/1997 | 57–61(83) | 1 | 4.5 | 4.91(84) | 1 | Open(85) | 1 | No(85) | 0 | Yes(32) | 1 |
Ruapehu | Full eruption: 17/06/1996 | 57.5–62(86) | 1 | 1.5 | 1.9(86) | 1 | closed(87) | 0 | No(87) | 0 | No(87) | 0 |
Eyjafjallajökull | Phase I/III on 14–19/04 & 05–18/05/2010 | 56.6–61.4(88) | 1 | 5 | 1.8(89) | 0 | Closed(90) | 0 | Yes(91) | 1 | No(92) | 0 |
Etna (1) | Full eruption: 28/10/2002 | 47(93) | 0 | 4 | 3.4(93) | 1 | Open(94) | 1 | No(94) | 0 | No(94) | 0 |
Popocatepetl | Climactic events on 10/03/1996 | 59.8–63.1(95) | 1 | 10 | 3.2(96) | 0 | Open(44) | 1 | Yes(44) | 1 | No(44) | 0 |
Etna (2) | Full eruption: 27/10/2002 | 47(93) | 0 | 4 | 3.4(93) | 1 | Open(94) | 1 | No(94) | 0 | No(94) | 0 |
Etna (3) | Full eruption: 24/11/2006 | 48(93) | 0 | 4 | 3(93) | 1 | Open(94) | 1 | No(94) | 0 | No(94) | 0 |
The five explicative variables considered here (SiO2 (P1) and H20 (P2) magma content, open or closed character of the conduit (P3), occurrence of phreatomagmatism (P4), and formation of co-PDC plumes (P5)) are coded as Boolean data type (0/1) to be used in the model selection analysis. The threshold between low and high SiO2 content is set at 56 wt% for P1. The threshold between low and high water saturation for P2 is set considering the inclusion entrapment depth. Missing data for P2 are compensated by the model.