The Reykjanes Peninsula is a fissure eruption zone, not a central cone volcano. Eruptions occur along linear crack systems driven by Mid-Atlantic Ridge plate divergence, producing effusive lava flows rather than explosive ash eruptions. The Fagradalsfjall and Svartsengi systems are the two primary active fissure systems in the current 2021-onward eruptive cycle. Volcanic gas emissions, particularly SO2, extend the hazard zone well beyond visible lava.
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