MadSci Network: Earth Sciences |
Well, it depends on what is your concept about a volcano... The largest volcanoes we have are underwater, separating the continents, in a region that we call "mid oceanic ridges". In North Atlantic, for example, in the middle of the ocean, between USA and Europe, the mid oceanic ridge goes from near the north pole to the equator. Iceland is formed by the lava of this volcanic system, and is a special case, where the volume of magmatic material was so big that it formed an island. Hawaii is another example, although it is not in the mid oceanic ridge, but over a hotspot. In these regions, the magma is continuously being erupted between rock fractures, and, in contact with the sea water, it becomes a solid rock, joining the adjacent ones and forming big structures. In South Atlantic, this mid oceanic ridge has about 135 million years of continuous activity. Best regards Eder C. Molina eder@iag.usp.br Dept. of Geophysics IAG-USP Brazil
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