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Nature 453, 1236-1238 (26 June 2008) | doi:10.1038/nature07075;
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Explosive volcanism on the ultraslow-spreading Gakkel ridge, Arctic Ocean
Roughly 60% of the Earth|[rsquo]|s outer surface is composed of oceanic crust formed by volcanic processes at mid-ocean ridges. Although only a small fraction of this vast volcanic terrain has been visually surveyed or sampled, the available evidence suggests that explosive eruptions are rare on mid-ocean ridges, particularly at depths below the critical point for seawater (3,000|[thinsp]|m).
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