It seems that although the Pacific 'Ring of Fire' [NZ - Japan - Alaska - Mexico - Chile]is well known for significant and persistent eruptions, to get something really big if less frequent you need to step a little to one side and look at Indonesia [Krakatoa, Tambora, Lombok as in the article; also Toba a long way back]. A different quality of magma? Deeper interaction betwen plates?
Indeed. Upper layer continental plate rocks are rich in
silicon and
Aluminum (SIAL), whilst oceanic plate rocks, underlying the SIAL are rich in
silica, iron, and
magnesium (SIMA) and is less viscous than the SIAL and depending on the mineral mix, this viscous property changes considerably as does the explosiveness of the volcanoes.
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Dave,Derby