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An estimated 17 million tons of SO2 gas were injected into the stratosphere by Pinatubo's high eruption cloud.
For example, ash particles that fall from a high eruption cloud to form widespread layers downwind from a volcanic eruption are referred to as tephra and not as a pyroclastic flow deposit.
Plume trajectories are not wind-affected at high eruption intensities and/or under weaker wind speeds.
We speculate that these high eruption rates are probably maintained by frequent replenishment by variably differentiated magmas from a parental source.
Although large basaltic stratovolcanoes tend to have high eruption rates and relatively constant repose intervals, these cases are not representative of the various types of volcanoes in Japan.
The TRC2 deposits are interpreted as the products of multiple, erosive, highly-inflated pyroclastic surges resulting from collapse of an unusually high eruption column relative to previously documented mafic phreatomagmatic eruptions.
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The density of anomalously high eruptions within the window surrounding the Range Front blind thrust is 3 6 times greater than outside this region.
On September 4, 2007, a 3 km-high eruption column dispersed ash up to 20 km from the summit (Vaughan et al. 2008).
However, there are periods with a higher eruption frequency than others.
The event with the highest eruption column (6 km above the crater; JMA, 2012) was observed on 13 March 2011.
The first two subplinian events were relatively long but included periods with a low eruption column, and each event ended with the highest eruption column.
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