What geologic significance does the Ring of Fire have?

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The Ring of Fire is a major area in the Pacific Ocean where many volcanic eruptions and earthquakes occur. This area is also called the circum-Pacific belt. The Ring of Fire is significant geologically because of the amount of seismic activity that happens in this area.

One reason this area is geologically significant is that over 90 percent of the world's earthquakes occur in The Ring of Fire. An earthquake is caused when the tectonic plates of the Earth shift. These plates move and collide in a variety of ways that can cause earthquakes.

Another reason The Ring of Fire is significant geologically is because of the amount of volcanic eruptions that occur in this area. There are more than 400 volcanoes in this area.

Due to the large amount of seismic activity, geologists have been studying this area since the 19th Century. The amount of earthquakes and volcanic eruptions that happen daily in this area provide ample possibilities for scientists to study seismic activity.

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There are at least two ways to express the geological significance of the Ring of Fire.

First, we can say that this area is geologically significant because it is so very seismically active.  This is an area of the world that is home to the majority of all the volcanoes in the world.  It is also where the majority of all the earthquakes in the world occur.  This means that it is very significant for geologists because they can observe a variety of seismic activity.

Second, we can say that this area is geologically significant because of its plate tectonics.  The seismic activity discussed in the previous paragraph is caused by plate tectonics.  There are subduction zones on both sides of the Ring of Fire.  As the oceanic plates slide under the continental plates, volcanoes are created as well as tensions that can lead to earthquakes. 

Thus, the Ring of Fire is geologically significant because of its plate tectonics and the seismic activity that the plate tectonics cause.

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