Preview

Types of Volcanic Eruptions and Tornadoes

Good Essays
Open Document
Open Document
486 Words
Grammar
Grammar
Plagiarism
Plagiarism
Writing
Writing
Score
Score
Types of Volcanic Eruptions and Tornadoes
Volcanic eruptions have caused some of the worst disasters in the world. They can wipe out entire cities and kill thousands of people. The name of volcano comes from Roman term. It derives from Vulcan which is the name of Roman fire god. Romans believed that Vulcan lived on a volcanic Italian coast. Romans called the island Vulcano.
According to scientists, volcanic eruptions are divided in to four basic groups. They are commonly known as Hawaiian, Strombolian, Vulcanian, and Peleean. The term of Hawaiian eruptions are named after the volcanoes in Hawaii. These volcanic eruptions are the least violent type. They produce highly fluid lava which flows quietly. This gradually builds up a shield volcano.
Strombolian eruptions are named after Stromboli. These result from the constant release of gas from the magma. As the gas escapes, it produces tephra that piles up, turning into a cinder cone. Strombolian eruptions happen when sticky magma plugs the central vent. This makes the magmatic gas build up pressure until it blasts. The magma is turned into volcanic dust and bombs.
Vulcanian eruption which comes from the ancient Roman belief, are more violent than the strombolian eruption. Vulcanian eruption happens and brings magma which is more viscous. Vulcanian explosions are usually larger and noisier than the Strombolian eruptions.
Paleean eruptions are famous as the most violent kind of volcanic eruptions. The name of Paleean comes from the eruption of Mount Pelee, Martinique in 1902. It killed almost 38 thousands people. A Peleean eruption occurs when the magmatic gas build up tremendous pressure. This causes violent explosions with glowing clouds of hot ash and dust.
Tornadoes are known as one of the most damaging disasters. A tornado is a very powerful column of winds which spirals around a center of low atmospheric pressure. A tornado will look like a large black funnel which hangs down from a storm cloud.
The name "tornado" derives from the Latin "tonare". It

You May Also Find These Documents Helpful

  • Good Essays

    viscosity such as basaltic lava then the eruption will not be that explosive, usually the…

    • 1097 Words
    • 3 Pages
    Good Essays
  • Satisfactory Essays

    Geology Chapter 5

    • 580 Words
    • 3 Pages

    An effusive eruption occurs when the magma feeding the volcano is hot and mafic causing it to have low viscosity. An explosive eruption occurs when pressure builds in a volcano. It may be a small explosion like a basaltic eruption where the gas builds up and suddenly escapes or it can be a large explosion which can be triggered by many things, such as cracks in the flank of an island volcano where water enters the magma chamber and turns to steam, or if a very viscous magma plugs the vent and the pressure increases so much it cracks parts of the volcano and…

    • 580 Words
    • 3 Pages
    Satisfactory Essays
  • Better Essays

    Script For Mt St Helens

    • 1103 Words
    • 5 Pages

    Coupled with these episodes were hundreds of small bursts or explosions of gas and steam. Mt. St. Helens has had four major eruptions and lots of minor ones. Volcanoes erupt due to the pressure of the magma and earth, and then erupts if a plate moves. Here is an image of the volcano before and after the eruption in…

    • 1103 Words
    • 5 Pages
    Better Essays
  • Good Essays

    Pavlof Research Paper

    • 589 Words
    • 3 Pages

    Volcanic eruptions can cause damage within hundreds of miles away. The volcano ash's causes airplane engines to fail, destroys crops, contaminates water, and damages electronics and machinery. When the ash touch's the ground, burying everything, sometimes even make's buildings to collapse. Mount St. Helen's produced more than 490 tons of ash that fell over some many miles. All volcanos are dangerous. They are all scattered all over the world and we don't know when they are going to blow. The three volcanos I picked were pretty interesting. The Pavlof is the most active and one of the most active in North America. The Cero Negro is not as big as the other to volcano's I picked. The Tungurahua is a very large and pretty cool looking volcano.…

    • 589 Words
    • 3 Pages
    Good Essays
  • Good Essays

    The type of magma affects the severity and type of volcanic processes that occur because where there is basic (basaltic) magma, that is low is silica thus has a low viscosity, trapped gas bubbles are allowed to expand freely as they rise to the surface. This means the eruption fluid is free-flowing and therefore cannot suddenly erupt explosively. On the other hand, where there is acid (andesitic and rhyolitic) magma, the silica content is high therefore it has a high viscosity meaning gas bubbles struggle to expand and the magma often solidifies before it reaches the surface. These solidified sills and dykes cause a blockage that leads to a build up of pressure and eventually to a violent explosion.…

    • 1598 Words
    • 4 Pages
    Good Essays
  • Better Essays

    A volcano is an earth hazard that occurs on faults between tectonic plates on a destructive boundary and an eruption is a natural disaster. A primary impact happens immediately after the disaster and before any response like death or collapsing or destruction of buildings. A secondary impact occurs later after the disaster, such less farm produce or a reduction in tourism. The severity of these impacts will differ considerably in a MEDC and LEDC where volcanic eruptions have taken place. These may be seen in the Mount St. Helen volcano eruption as well as in the Iceland volcanic eruption. They may also show that the impacts vary from volcano to volcano, place to place.…

    • 1025 Words
    • 5 Pages
    Better Essays
  • Good Essays

    Primary hazards that are associated with volcanoes include; pyroclastic flows, Tephra, Lava flows and volcanic gases. Pyroclastic flows are waves of very hot gases and tephra with flow with high velocities. The pyroclastic flow that was seen at the eruption of Mount St Helens, USA in 1980 was a result of dense gas and ash combinations. It travelled a total of 25km north of the volcano and had a top temperature of 700’c. The flow was slowed down by ridges around the volcano but it contributed to a $450 million in damages to forestry.…

    • 571 Words
    • 2 Pages
    Good Essays
  • Good Essays

    One factor that heavily influences how hazardous a volcano is, is the plate boundary that it lies on. Subductive plate boundaries tend to produce much more violent eruptions than conservative or constructive margins. Subductive boundaries occur where two plates (one continental and one oceanic) are moving toward each other. The denser plate, the oceanic, is forced underneath the continental. As it subducts into the asthenosphere, it begins to turn back into magma. This magma is light and less dense than the asthenosphere, so it rises and forces its way through weaknesses in the crust. This is how volcanoes are formed on subductive margins. An example, is the Aleutian Islands which are a chain of volcanoes formed by the subduction of the pacific oceanic plate underneath the Eurasian/north American (?) plate.…

    • 627 Words
    • 2 Pages
    Good Essays
  • Better Essays

    Pompeii Research Paper

    • 1091 Words
    • 5 Pages

    Volcanoes are formed on land near coastal areas when a continental plate and an oceanic plate converge. The oceanic plate submerges, due to its higher density, and is pushed deeper and deeper beneath the surface. The high temperature and pressures below melt the rock which creates hot, buoyant magma. Ultimately this magma rises towards the surface and accumulates in a reservoir, known as the magma chamber. The eruption occurs when the pressure within in the chamber surpasses the pressure of the upper rock, magma forces its way through the cracks in Earth’s crust. Magma that is low in gas and silicon dioxide produces thin quickly spreading lava which has a low viscosity, while a magma that is heavily composed of gas and silicon dioxide will yield a thick, viscose magma. The thicker magma builds up and because of this pressure, will cause a large…

    • 1091 Words
    • 5 Pages
    Better Essays
  • Good Essays

    The third event that can be expected when Mt. Thunder erupts is a pyroclastic flow. Pyroclastic flows are created when tephra fragments and volcanic gas flows down valleys on the flanks of volcanos. Pyroclastic flows are composed of extremely hot fluidized mixture of gas and rocky fragments that typically move faster than 100 miles per hour. These are the most deadly of all volcanic phenomena which can be seen when looking at the devastation a pyroclastic flow caused when it killed 28,000 people in the city of Saint-Pierre.…

    • 753 Words
    • 4 Pages
    Good Essays
  • Powerful Essays

    One factor that must be considered is the viscosity of the magma. The viscosity can determine how violent the eruption is and what shape the volcano becomes. Viscosity can be affected by temperature, dissolved gases in the magma and its silica content. High temperatures can make the magma less dense allowing it to flow more easily. The amount of dissolved gases lowers the viscosity. Lastly a high silica content will make the magma more viscous. Magma of a high viscosity can cause very violent eruptions. These pose the greatest threat as there very destructive. This is because it has a tendency to plug the volcano, trapping gasses which build pressure and eventually erupt violently. This can mean that the eruptions caused by thick magma can be less frequent and more difficult to predict, meaning that when an eruption does occur, it is usually with little or no warning, which can lead to catastrophic consequences as any nearby settlement will be relatively unprepared for the effects of a violent volcanic eruption. It also more likely to produce clouds of smoke and ash which can lead to suffocation and is a big killer during eruptions. You then have your thinner, less viscous magma such as AA or pahoehoe. It has a very high temperature, 950 C. It moves quickly due…

    • 1538 Words
    • 4 Pages
    Powerful Essays
  • Better Essays

    Common volcanic hazards include: Pyroclastic flows, Ash clouds and mudslides. Pyroclastic flows are high-density mixtures of hot, dry rock fragments and hot gases that move away from the vent of the volcano at high speeds. They can reaches speeds moving away from a volcano of up to 450 mph and the gas can reach temperatures of about 1,000 °C. They will catch fleeing victims and kill them instantly thus making them a devastating hazard. Volcanic ash is formed during explosive volcanic eruptions when dissolved gases in magma expand and escape violently into the atmosphere. They can also have devastating effects due to the similar heat as pyroclastic flows. They have secondary effects as well, such as stopping air travel simply because it is unsafe. Navigation is difficult and the cloud is still dangerous. The fine ash erupted from explosive volcanoes can cause destructive mudflows. When a volcano erupts, ice and snow melted by the heat of the eruption run downhill carrying ash particles and other debris. They can flow tens of metres per second, be 140 metres deep, and destroy any structures in their path.…

    • 1382 Words
    • 4 Pages
    Better Essays
  • Satisfactory Essays

    Mt St Helens was the most disastrous volcanic eruption in US history. 57 people died, more than 200 homes were lost and more than 200 miles of roads and railways were damaged. This Stratovolcano is rated a 5 on the explosivity index. Like The eruption of Mt St Helens, Mt Vesuvius was the biggest catastrophic eruption in European history. 13,000 people died and Two Cities were utterly destroyed (Pompeii and Herculaneum). Mt Vesuvius Is the only active volcano on the European mainland. Mt Vesuvius is one of the deadliest eruptions ever. Mt Vesuvius ejected about 12 miles of debris into the air, about double the size of Mount Everest. Then a searing combination of pumice and ash of up to 1300 degrees Fahrenheit hit the city at 70 miles an hour.…

    • 243 Words
    • 1 Page
    Satisfactory Essays
  • Satisfactory Essays

    Volcanos are mighty mountains that rise from the ground but these beautiful beast come with a catch. When they “wake up” they can tear a whole island or town to pieces and pieces. Most volcanoes cause tons of destruction including flames and lava when awakened this roaring beast isn’t so peaceful.…

    • 469 Words
    • 2 Pages
    Satisfactory Essays
  • Good Essays

    Volcanoes exist all around the world. There are three types of volcanoes, they are shield volcano, cinder cone volcano and a composite volcano. A volcano is a place where ash, gases, and molten material rock from deep underground erupt to the surface. Lava comes out of a vent , then it turns into a lava flow. When external waters, such as groundwater , mixes with magma and then it turns into steam. The violence of an eruption depends on the amount of gas that was dissolved in the magma. Pyroclastics, form from when fragments of magma are thrown into the air by expanding gas. silicic caldera complexes produce the most violent volcanic eruptions.…

    • 467 Words
    • 2 Pages
    Good Essays

Related Topics