![]() The shapes and textures of lava formed by submarine volcanoes are different from lava erupted on land. The presence of water can greatly alter the characteristics of a volcanic eruption and the explosions of underwater volcanoes in comparison to those on land.įor instance, water causes magma to cool and solidify much more quickly than in a terrestrial eruption, often turning it into volcanic glass. Hydrothermal vents, sites of abundant biological activity, are commonly found near submarine volcanoes. Only 119 submarine volcanoes in Earth's oceans and seas are known to have erupted during the last 11,700 years. The total number of submarine volcanoes is estimated to be over one million (most are now extinct) of which some 75,000 rise more than 1 kilometre (0.62 mi) above the seabed. Although most submarine volcanoes are located in the depths of seas and oceans, some also exist in shallow water, and these can discharge material into the atmosphere during an eruption. The volcanoes at mid-ocean ridges alone are estimated to account for 75% of the magma output on Earth. Many submarine volcanoes are located near areas of tectonic plate formation, known as mid-ocean ridges. Submarine volcanoes are underwater vents or fissures in the Earth's surface from which magma can erupt. ![]() Circular plumes from a submarine eruption near Tonga
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