classes according to their eruption of a volcano
Wednesday, May 30, 2007
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-Strombolian: The lava is flowing with abundant and violent landslide gases. Because gases can be released easily, not form ash. When the lava falls at the edges of the crater down the slopes and ravines, but does not reach such length as Hawaiian.
-Vulcan: In this type of volcanoes emit large amounts of gas a little fluid magma. That's why the explosions are very strong and pulverized lava, producing a large amount of ash that is released into the air with other fragmentary materials. When ejecting lava, it is rapidly consolidating, but that release gases break the surface. So it's very rough and very irregular.
-Vesuvian: The gas pressure is very strong and very violent explosion occurs. Pyroclastic cloud that produces precipitation of ashes cooled.
-Fight: The lava is very viscous and is consolidating rapidly. Comes to cover the entire crater. The enormous pressure of the gases that are out, lift this cap to form a large needle cam.
-KRAKATOANO: Originates tremendous explosions and huge tidal waves.
-ERUPTIONS OF ONE HUNDRED: The large craters are converted during the period of repose of the volcano in huge lakes are covered with snow. Regaining volcano activity, water mixed with ash and debris is released forming torrents and avalanches of mud that destroyed everything in their path.
-eruption fissure: Those that originate along a break in the earth's crust and can be several kilometers. The lava flowing along the fracture are smooth and cover great expanses forming broad plateaus with more than a mile thick and thousands of square kilometers.
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