Construct · 1 fields · 1 citations
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A phreatomagmatic eruption is an explosive eruption driven by the interaction of rising magma with external water (groundwater, a lake, or the sea), in which rapid heat transfer flashes the water to steam and shatters the magma into fine fragments. Sheridan and Wohletz's 1983 review of hydrovolcanism set out how the ratio of water to magma controls the violence and the fine, often blocky, ash such eruptions produce. The referent is an eruption style defined by magma-water interaction, distinct from purely magmatic explosivity driven by the magma's own dissolved gas.[1]
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