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Volcano Facts Essay Research Paper Hot

Volcano Facts Essay, Research Paper


Hot! Fire! Destruction! These are words that most


people associate with volcanoes. But some good effects can


come out of volcanoes. Volcanoes also have their own


special mythology associated with them. A lot of volcanoes


have some general characteristics in common. There are many


volcanoes around the world and some have special


characteristics. So come along and take a trip with me into


the wonderful and exciting world of volcanoes.


Over 550 volcanoes have erupted on the surface of the


Earth since human kind has been able to record history.


Their destructiveness has claimed the lives of over 200,000


people during the last 500 years with 26,000 deaths between


1980 and 1990 alone. They have also cause an innumerable


amount of property damage.


The biggest eruption of the twentieth century was the


eruption of Novarupta on the peninsula of Alaska. The


amount of lava that erupted measured to roughly 15 cubic


kilometers! All of the lava erupted equaled to the amount


of 30 times the amount of lava that came from Mount Saint


Helens and it is also the equivalent of 230 years of


eruptions at Mount Kilauea. The eruption lasted for 60


hours on June 6, 1920.


The biggest eruption, despite its size, was not the


most destructive, for the most destructive was the eruption


of Mount Saint Helens in Oregon during the week of May 18th,


1980. This eruption mainly caused just loss of property,


because many people didn?t expect the volcano to erupt.


Although some people did die, this volcano was kind of weak


compared to the size of the eruption and amount of lives


lost in other eruptions like Tambora, Indonesia in 1815


where 92,000 people died.


Despite all of these bad effects, some life still


shines through these tragedies. For example the ash that a


volcano spews out covers many square miles of plants and


trees. This holds in water and waters plants. The ash also


contains many nutrients that plants use. A little more than


80 percent of the Earth?s surface is volcanic in origin,


meaning that most of the Earth?s surface was formed by


volcanoes. Also, magma deposits heat water underground


which produces geothermal energy.


The word volcano comes from an island off of the coast


of Sicily called Vulcano. The people of Sicily thought that


the clouds of dust and spurts of lava were made from Vulcan,


the blacksmith for the Roman Gods. They believed that


Vulcan forged thunderbolts for Zeus and weapons for Mars on


that island.


Out of the 550 of the world?s active volcanoes, the


world?s largest active volcano is Mauna Loa, it is one of


the Hawaiian islands. The island protrudes around 13,677


feet above sea level; while the whole island was formed by


an underwater volcano, this brings it 28,000 feet above the


ocean floor where it started. From the base underwater to


the summit above water, this volcano stands higher than


Mount Everest.


There are two main types of volcanoes out there in the


world today, the first is fel

sic, and the second is mafic.


Felsic volcanoes have a high silica content and a light


color to the lava. The second, mafic, has just the


opposite, a low silica content and a darker color.


Then there are underwater volcanoes and above ground


volcanoes. The underwater volcanoes are less known about


than above ground for the obvious reason that they are seen


when they are above ground. Underwater volcanoes produce


some things called black smokers, they are basically just


ash as well as black smoke that combine and heat up water to


boiling temperatures. An interesting fact about underwater


volcanoes is that some islands have been formed by lava


eruptions building up year after year. An island chain that


is very well known that has been formed by this process is


the chain of the Hawaiian Island chain. This chain also


includes the world?s largest volcano, Mauna Lao, which, when


you count the amount underwater and the amount above water


is taller than Mount Everest.


Some volcanoes have been found in our solar system that


are not on the planet Earth. One volcano, which is the


largest one in our solar system, is Mount Olympus Mons on


the planet Mars. This is the only volcano found on the


planet mars. There are also numerous volcanoes found on Io,


a moon of the planet Jupiter. These volcanoes also show


that some plate tectonics on Io, even though no plate


tectonics is believed to have occurred on Mars.


Volcanoes form when magma, melted rock underground (it


is called lava when it reaches the surface) (most of it


forms around 50 to 100 miles underground), when the magma


mixes with gas and rises, pressure builds against the


surface, the magma breaks through and you get a volcano.


Shield volcanoes form when a lot of lava spills out of


a vent and goes in a broad, flatter area. Another type of


different volcano is a cinder cone. Cinder cones are made


when tephra, thick globs of magma, erupts from a vent in the


ground and comes back down then accumulates. A famous one


is Paricut?n in western Mexico. It started to form in 1943


in the middle of a farmer?s corn field, then it started to


stop in 1952. When it was finished, the cinder cone was


1,345 feet higher than the base. Then there are composite


volcanoes which form when tephra and lava erupt from the


same vent. One example of this is Pompeii and Japan?s Mount


Fuji.


When all of the magma is drained out of the chambers of


the volcanoes, called magma chambers, sometimes the volcano


can?t support itself and collapses, this leaves a crater


called a caldera.


So, I hope that you have learned about some specific


volcanoes as well as the properties that go along with them


(even if they are bad). I also hope that you found out that


volcanoes aren?t all that bad.


World Book Encyclopedia, Book U-V, pg.462-pg.467


Internethttp://vulcan.wr.usgs.gov/LinvingWithVolcanoes/Facts/misc_volcanic_facts.htmlhttp://volcano.und.edu/vwdocs/vw_hyperexchange/deadly_volcs.htmlhttp://volcano.und.edu/vwdocs/eruption_scale.htmlhttp://infoplease.lycos.com/ipa/A0001746.html

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