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Mount St Helens Research Paper

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Ask anyone in the Pacific Northwest to name a volcano in the area and you will most likely get the response of “Mount St. Helens”. There is good reason for this particular volcano to have gained such a great reputation for itself, and that is the eruption which occurred in 1980. Beginning in March, new systems of seismographs were being implemented to track the size of earthquakes that were happening in the St. Helens area. Earthquakes were recorded up to three times a day almost daily and on March 27th, an official warning was sent out as one of the quakes caused a stream of ash over 6,000 feet into the air. On the morning of May 18th, 8:32am, an earthquake measuring in at a magnitude of 5.1 on the seismograph signaled the beginning of the eruption.
Shortly after the eruption, the entire northern side of the volcano collapsed (caused by the collapsing of the crypto dome) which sent an estimated 2.5 cubic kilometers of materials sliding the side of the mountain. This collapse released superheated gases along with magna that had been trapped in a lateral explosion. Anything within eight miles of this blast was gone instantaneously and continued on for …show more content…

Helens, put shortly, is due to the Juan De Fuca plate sub-ducting beneath the North American plate. The collision between these two plates caused the formation of multiple mountain ranges/volcanoes, St. Helens included. As the Juan De Fuca plate moves deeper and deeper south, it starts to get hotter and hotter. Once it reaches the upper mantle (Asthenosphere), the plate begins to melt into magma while at the same time, water is being introduced as well. This combination increases the volume of the magma, thus, decreasing the density, causing it to start moving upwards through the lithosphere until it reaches the surface. This process takes hundreds of thousands of years, resulting it huge volcanoes named Stratovolcanoes, capable of mass destruction as St. Helens so kindly

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