Table 2 Umbrella cloud radii and VEI indexes of severala observed and bpast eruptions.
From: The radius of the umbrella cloud helps characterize large explosive volcanic eruptions
Eruption | VEI | Volume (km3) | Radius (km) |
|---|---|---|---|
Calbuco, Chile, 2015a | 4 | 0.58 bulk volume63 0.38 bulk volume64 | ~50–6063 |
Kelut, Indonesia, 2014a | 4 | 0.1 bulk volume65 | ~40 (upwind)66 |
Grímsvötn, Iceland, 2011a | 4 | 0.6–0.8 bulk volume 0.2–0.3 DRE67 | ~25–5067 |
Cordón Caulle, Chile, 2011a | 4–5 | 1.1 ± 0.2 tephra fallout volume27 | ~35–60 (crosswind)27 |
Sarychev Peak, Kurile, Russia, 2009a | 4 | 0.4 bulk volume68 | ~2569 |
Okmok, Alaska, U.S., 2008a | 4 | 0.26 DRE70 | ~32.571 |
Manam, Papua New Guinea, 2005a | 4 | – | ~9072 |
Reventador, Ecuador, 2002a | 4 | 0.3 bulk volume73 | ~42.571 |
Pinatubo, Philippines, 1991a | 6 | 8.4–10.4 bulk volume74 3.7–5.3 DRE74 | ~250 (upwind)75 |
Redoubt, Alaska, U.S., 1990a | 3 | – | ~17 (co-ignimbrite cloud)57 |
Mount St. Helens, U.S., 1980a | 5 | 1.3 tephra fallout volume76 0.73 tephra fallout volume77 | ~15 (upwind)78 |
Tambora, Indonesia, 1815b | 7 | ~100 tephra fallout volume79 | ~50079 |
Campanian eruption, Italy, ~40 ka B.P.b | 7 | ~210 tephra fallout volume56 | ~43056 |