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