The Ring of Fire.

Most vol piece of assoes argon located on the continents edges, on island chains or beneath the sea forming long messiness ranges. more than than one-half of the worlds active volcanoes above sea train circulate the peaceful Ocean to form the circum- pacific resile of Fire. The ragtag and bobtail of fire makes up seventy five percent of the worlds dormant and active volcanoes. More than half of the worlds active volcanoes above sea level are part of the call in. The evade of Fire is an firing of volcanoes that stretches from New Zealand in all the way across the soaring of North and South America. This realm got its name because on that slur is a outstanding amount of volcanoes that encircle the peace-loving Ocean. The ring of fire is known for frequent earthquakes and volcano eruptions. This area of volcanic and seismic activity was noticed and exposit before the maneuver of the plate tectonics theory. Around the ring of fire the Pacific plate is colliding wi th and sliding underneath former(a) plates. This area is known as the subduction zone. The button that is generated by these plates is tremendous. The Ring of Fire is the location where close of the seismic activity in the world is taking place. The Pacific Ocean has a mid- marine ridges and is surrounded by subduction zones.

The diffusion rates of the ridges are very fast, resulting in the subduction zones destroying a groovy amount of the Earths crust. This is why there are so galore(postnominal) earthquakes and volcanoes all around the border of the Pacific Ocean, where the subduction zones are located. T he energy is so great that it can easily mel! t rocks into magma. The Ring of Fire is a great example of plate barrier volcanoes. The major volcanic regions in the Ring of fire are: the Cotopaxi and Azul volcanoes... If you want to get a full essay, order it on our website: OrderCustomPaper.com

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