Volcanoes occur in many different places. Most places volcanoes occur on the edge of the tectonic plates. Volcanoes are formed by the earth’s plates moving closer and closer pushing each other up. Volcanoes are one of the most frightening and dangerous events on earth. A volcano I an opening in earth's crust, by molten rock and gas.Most of the Earth's volcanoes are located around the Pacific Ring of Fire because that the location of most of the Earth's subduction zones.When lava erupts it is made up of a slush of crystals, liquid, and bubbles. The liquid freezes to form volcanic glass. Chemically lava is made of the elements silicon, oxygen, aluminum, iron, magnesium, calcium, sodium, potassium, phosphorus, and titanium. There are 4 different types of volcanoes.There are Extinct, Dormant, Active and Mud volcanoes. The most popular volcano an Active Volcano. An Extinct Volcano is when the magma under the surface colls. Most Extinct Volcanoes have not erupted for thousands of years. Dormant Volcanoes are ones that are quiet for a long and suddenly erupt again without anyone knowing or realizing it was going to happen. When a volcano has not erupted for …show more content…
Volcanoes are mainly formed by plate tectonics. Volcanoes are closely associated with plate tectonic activity. Volcanoes mainly vent from the vents crust. Most magma is formed by partial melting of the mantle. Volcanoes are made up of different layers of the earth. Many things can occur after a bad eruption. There are 3 main things that can happen. They are Hot Springs, Calderas and Mud spots.Hot Springs occur when magma beneath the surface heats up the water in the cracks overlying rocks. Calderas happen when a massive blast of lava empties a volcano's magma chamber and causes the volcano to collapse on itself. Mud spots happen when water is heated underground can release steam that forces its way to the
About three-quarters of Japan is mountainous. They were formed by tectonic plates colliding. Volcanoes were formed by the land breaking, and the liquid rock built up in it. A lot of the volcanoes are active, yet no one knows when one will erupt. The
Basalt forms due to the partial melting of the layer of the mantle called the asthenosphere. The asthenosphere is the plastic zone of the mantle beneath the rigid lithosphere. Mantle plumes coming from the mesosphere can cause the asthenosphere to melt with heat or even if pressure decreases, which is called decompression melting (Richard 2011). The magma that forms from this melting is mafic magma that solidifies once it reaches the earth’s surface and cools quickly. The above process mainly occurs mainly during intraplate igneous activity which is the main explanation for volcanic activity that occurs a long distance away from a plate boundary. If the tectonic plate above the mantle plume is moving it can create a string of volcanic activity such as in Hawaii. See Fig 2.
The most iconic volcanic eruption in history was the eruption of Mt. Vesuvius in 79 A.D. Mt. Vesuvius is located on the west coast side of Italy. Pompeii was the ancient town five miles from Mt. Vesuvius where people would flock to the area in 79 AD to be near the Bay of Naples. Little did they know that the volcano would erupt into the most destructive volcano in history. Mt. Vesuvius has erupted about three dozen times and was the most disastrous due to the large population around the area. The volcano, which is still active today, is a stratovolcano. A stratovolcano has pyroclastic flows and erupt explosively and violently. Pyroclastic flows don't necessarily look exactly like “flowing eruptions”. These eruptions are not the “flowing” type of eruptions because they are eruptions with explosions and blowing clouds that fill the air. These clouds are usually dark clouds that are made up of ash. Pompeii had some signs of the volcano erupting, but the technology was not like the technology of today where scientists can monitor the volcanic activity.
Volcanoes form in destructive and constructive areas on Earth. They form when plates in Earth’s core (tectonic plates) force molten rock, gases and ash to Earth’s upper mantle.
Volcanoes have played a key role in forming the face of the earth as we know it today. Some of the most well known landmarks and locations in the world are volcanoes. From the Hawaiian Islands to Mount Vesuvius, the Earth is populated with hundreds of active and dormant volcanoes. Among these volcanoes there are multiple different types. Stratovolcanoes, the most dangerous type of volcanoes, are built by multiple eruptions over many years. Shield Volcanoes, the largest recognizable volcanoes, are characterized by being short but very broad with low sloping sides. Cinder cones, the most common type of volcano in the world, are composed of large amounts of tephra, or pyroclastic debris. The last type of volcano is supervolcanoes. Supervolcanoes are the largest volcanoes. They also have the highest potential for damage. This paper will discuss these these different types of volcano.
The eruption on Mount Saint Helens has a specific cause and comes with many effects. A multifold of people would say that the “mountain looked like the site of an atomic blast” (Bredeson 30). That is a very accurate depiction as it took great power to inflict as much damage as it did. The reason for this impressive amount of force is that when magma is built up with pressure and an earthquake hits, the pressure gets magnified and the volcano explodes (Lewis). This is exactly what happened inside Mount Saint Helens. Furthermore, it has been revealed that “The earthquake that triggered the explosion was a 5.2 on the Richter scale” (Gunn 559). The earthquake to the magma can be compared as a match to gasoline. Even though the earthquake was not huge, the scale of the eruption was much greater than that of the earthquake (Gunn 560). The earthquake was only the trigger that allowed for more devastating things to occur. Thirteen hundred feet of the volcano were lost in the explosion followed by landslides, mudslides, and lava flows...
Earth has physically changed millions of times due to moving tectonic plates which has formed our planets mountains; altering the way our environment looks. Volcanoes, (formed when magma from the upper mantle heads to the surface, causing the land to rise) are one of nature’s finest spectacles. These geographical forces have erupted many times; from small-scale eruptions to cataclysmic ones; making them a force to consider about. Therefore the past is useful in predicting possible future eruptions as in terms of the effects they can have on civilisation, they are unpredictable in what they can produce.
Volcanos are extraordinary geographic things. In Sioux City Iowa we do not have any volcanos. In fact we do not have any in the United States, but we do have some in Hawaii. A volcano works by the lower density of the magma relative to the surrounding rocks cause it to rise. Bubbles start to form from the gas dissolved in the magma. The bubbles exit in the magma with great pressure. Pressure helps bring magma to the surface or over the surface. Sometimes with tremendous pressure. Nevado Del Ruiz Volcano Eruption 1985 included many details common to volcano eruptions and caused damage and destruction to property and lives that affected
Volcanoes can cause damage by spewing lava, but earthquakes before the eruption can also cause damage. These earthquakes open fissures and let magma out to the surface. When the magma exits these fissures, streams of lava up to hundreds of feet can shoot into the air. The picture below shows the lava erupting from the fissures created by the earthquakes in...
Stories about volcanoes are captivating. Myths come in different versions, but all of them are capable of capturing yours, and everybody’s imagination.
Volcanoes are one of natures most interesting and dangerous phenomenons. The way volcanoes operate can be understood, on a basic level, by just some simple physics and chemistry, this paper will investigate and explain some of the basic physics that govern the behavior of volcanoes.
Since the dawn of history, volcanoes have been an awe inspiring feature of the earth that has frightened and intrigued mankind. Volcanoes have taken the lives of over 250,000 people in the last three hundred years and changed the lives of millions of others, but up until recently humans have had very little understanding of the volcanic processes that presage an eruption. The advent and implementation of new technologies and scientific methods has allowed us to begin to comprehend the inner workings of one of nature's most powerful forces. Through understanding how volcanoes work, volcanologists hope to accurately predict when an eruption may occur, what the magnitude and type of eruption will be, and what effect it will have on the surrounding area. Accomplishing this daunting task will ensure that in the future when an eruption occurs, the population at risk will be prepared and lives can be saved.
Volcanoes can be one of the most destructive forces on Earth. It is estimated that some
Igneous rocks are formed from the ejection of earth’s volcanoes. Deep down inside earth’s mantle there lies hot magma. Magma is molten rock that is kept below the surface. This mixture is usually made up of four parts: a hot liquid substance which is called the melt; minerals that have been crystallized by the melt; solid rocks that have made themselves tangled in the melt because of loose materials, and finally gases that have become liquid. Magma is created by an increase in temperatures, pressure change, and a alter in composition. When this magma is ejected from earth’s crust it earns a new name called lava. The lava hardens and becomes an Igneous rock.