Analysis of the frequency-size relationship of explosive volcanic erup
tions for the past 2000 years reveals that the time-averaged eruptive
mass flux of tephra from subaerial explosive eruptions is 3x10(4) kg s
(-1). This mass flux corresponds to a thermal energy release of 4x10(1
0) W. Half of the long-term (>10(3) year) mass and thermal energy rele
ase from explosive volcanic eruptions is accounted for by eruptions of
>10 km(3) of tephra.