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VOLCANOES

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Volcanoes are one of the most powerful forces on earth, along with earthquakes. They are our link to what is below the surface of the earth. Everyday, we are learning more about them, learning about their dangers and wonders.


Scientists have become more and more accurate with predicting when a volcanoe is going to erupt. They have identified many of the signs that poin to an upcoming eruption. Observing the state of a volcanoe happens during an eruption , or between eruptions. Before an eruption the volcanoe 'bloats' as magma enters it's resevoir and emits gases.

This cross section of the volcano outlines how the volcanoe swells up before erupting

This changes the volcanoes shape. The 'inflation' process can take from hours to days up to even a year. After the eruption, the volcanoe shrinks back to it's previous state. Scientists have been coming up with precise surveilance to monitor volcanic activity since 1948

Where are Most of our Volcanoes

A subduction zone volcano are volcanoes that appears on a subduction zone. (The name obviously gives it away) You will notice that almost all volcanoes show up on a subducion zone. When the earth's crust sinks into the mantle, it melts, creating magma, which is less dense than the solid crust, so it pushes up from the cracks. This forms the ocean trenches which volcanoes show up behind. The most volcanically active area on earth is the Ring of Fire. It is formed by the converging and diverging

of the pacific plate with the continental plates around it, forming a ring of subduction zones. Massive underwater trenches are formed from the plates submerging into the mantle. The largest is 11km deep, called Mariana's Trench. It's located off the east coast of the Phillipines. Of the some 550 volcanoes on earth, most of them are located on the subducting plates of the Ring of Fire. Volcanoes rarely form along transform plate boundaries because no gaps are created to allow magma to escape. This is diagram of diverging plates


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