Why do some volcanoes erupt explosively and others flow gently?
Because of the viscosity of the magma and how much dissolved gas it contains — and both are determined largely by silica content, which in turn depends on the tectonic setting.
The mechanism. Magma contains dissolved gases, principally water vapour and carbon dioxide, held in solution by pressure. As magma rises, pressure falls and the gas comes out of solution — exactly as it does when a bottle is opened.
What happens next depends on whether the gas can escape.
Low-viscosity (runny) magma lets bubbles rise and escape easily. Gas leaves gently, and the eruption is effusive — lava flows out. Dangerous to property, rarely to life, since you can walk away from most lava flows.
High-viscosity (sticky) magma traps the bubbles. Pressure builds until the magma fragments violently, producing an explosive eruption: ash columns, pyroclastic flows and volcanic bombs.
What determines viscosity. Principally silica content. Silica forms chains that make magma sticky:
Basaltic magma — low silica, low viscosity, hotter. Produces effusive eruptions and shield volcanoes with gentle slopes, as in Hawaii and Iceland.
Andesitic and rhyolitic magma — higher silica, far more viscous, cooler. Produces explosive eruptions and steep-sided stratovolcanoes.
Why the tectonic setting decides it:
Divergent boundaries and hotspots produce magma derived from the mantle — basaltic and runny.
Subduction zones produce magma that has interacted with water-rich sediment and continental crust, becoming enriched in silica and volatiles. This is why the Pacific Ring of Fire is explosive — it is a chain of subduction zones.
Water content raises explosivity independently, and magma meeting groundwater or seawater produces violent phreatomagmatic eruptions.
The Volcanic Explosivity Index (VEI) measures eruption size logarithmically, by volume of material ejected and column height.
What actually kills people: rarely lava. Pyroclastic flows — fast-moving currents of hot gas and ash — are the principal cause, along with lahars, mudflows of ash and water that can travel far from the volcano long after an eruption.