Preview

Earthquake and Its Effect

Good Essays
Open Document
Open Document
883 Words
Grammar
Grammar
Plagiarism
Plagiarism
Writing
Writing
Score
Score
Earthquake and Its Effect
Natural Hazards
What is a natural hazard?
A natural hazard is a naturally occuring physical event which poses a threat and negatively impacts people and the environment. Examples of natural hazards are: earthquakes, tsunamis, wildfires, floods, volcanic eruptions etc.

Earthquakes and their Occurence
What is an Earthquake?
An earthquake is a sudden rapid vibration along the earth’s crust due to individual tremors, sometimes causing great destruction to the earth’s lithosphere and its inhabitants. Earthquakes occur both on land and sea.They may occur at areas where plates collide (subduction zones/ convergent plate margins) ; where plates slide past eachother along fault lines (transform plate margins) or due to volcanic eruption.
Earthquakes may be of three different categories: * Tectonic – movement in the earth’s crust due to sudden movement along fault lines. * Plutonic - occurs deep within the subduction zone of colliding plates. * Volcanic – earthquakes accompanied by molten lava and gases.
Earthquakes may be of different intensities which determines how much damage it causes to life and property. The intensity of an earthquake is recorded by seismographs which are measured by the Mercalli Scale. The Richter Scale measures the magnitude of the earthquake.
How do Earthquakes Occur?
At a Zone of Convergence:
At a zone of convergence, tectonic plates move towards each other causing collision. A denser oceanic crust sinks beneath a less dense continental crust to form a subduction zone. Where plates collide at subduction zones plate edges are destroyed. This collision is associated with seismic/earthquake activity.

At Transform Plate Margins:
At transform plate margins tectonic plates slide parallel to each other, but in opposite directions causing a build up of friction. This friction causes plates to jerk and snap triggering an earthquake.

Volcanic Eruption:
Earthquakes produced by stress changes in solid rock due to the



Bibliography: * http://www.loc.gov/preservation/emergprep/earthquake.html * http://en.wikipedia.org/wiki/Earthquake_prediction * http://en.wikipedia.org/wiki/Natural_hazard * New Caribbean Geography( Vohn A.M. Rahil) * http://www.mona.uwi.edu/cardin/virtual_library/docs/1108/1108.pdf

You May Also Find These Documents Helpful

  • Good Essays

    Plate tectonic theory is a widely excepted theory that the Earth’s lithosphere is made up of plates, both oceanic and continental, which slowly move due to convection currents in the mantle and the asthenosphere. However, it is very hard to be certain as we can’t see the structure of the Earth, so some people do not agree with it. This theory saw the introduction of what we know today to be tectonic plates. Tectonic plates occur where there is radioactive decay in the core and temperatures are extremely high. This decay can occur anywhere in the earth’s core. This results in a plume of magma rising through the mantle creating a thermal current. When this current reaches the surface it spreads through the asthenosphere, before cooling and sinking. These are the convection currents which move tectonic plates. Convection currents will only occur in liquid form and in warm conditions. Tectonic plate theory has evidence to prove that these currents do take place. We know that the mantle is liquid and has high temperatures as magma that originates in the mantle is molten. This means that convection currents can occur. This part of plate tectonic theory is supported by global seismic activity because if convection current did not exist and plates were not able to move, earthquakes would not occur at any plate boundaries, but particularly at collision plate boundaries as there would be no plate movement.…

    • 942 Words
    • 4 Pages
    Good Essays
  • Powerful Essays

    Tectonic plates are powered by convection currents, which is the circular movement of magma within the mantle. These currents are powered by the core, which heats the magma, causing it to rise, cool and fall back down. This circular motion causes the plates, which float on the mantle, to move. The individual plates are separated by fault lines which extend from the surface all the way to the asthenosphere, at which point the fault disappears due to the plasticity of the rock that exists there. The earth’s plates are moved by convection currents in the mantle caused by localised concentrations of radiation and heat from the earth’s core. The plates are constantly in relative motion to each other, but this motion is extremely slow due to the incredible amount of mass being moved, friction, and the high viscosity of the asthenosphere. Where the different plates meet is called a plate boundary.…

    • 1864 Words
    • 8 Pages
    Powerful Essays
  • Good Essays

    The theory of plate tectonics explains the structure and motion of the Earth’s lithosphere. The theory states that the Earth’s crust is split into large sections called tectonic plates, and these move relative to one another creating boundaries at which the plates converge, diverge or move past each other. These plates are either continental or oceanic and are powered by convection currents, which is the circular movement of magma that comes from within the mantle. These currents are powered by the core, which heats the magma, causing it to rise, cool and fall back down. This circular motion causes the plates, which float on the mantle, to move.…

    • 1105 Words
    • 5 Pages
    Good Essays
  • Powerful Essays

    Earthquakes are an example of seismic activity caused by the build-up of tension at the three types of plate boundaries: destructive, constructive and conservative. The pressure is suddenly released as the plates jerk past each other, sending out seismic waves from the focus that travel through different parts of the earth. The movement of convection currents within the Earth’s mantle causing the crust to become mobile which creates the different types plate margins, makes the cause due to physical factors. However human activity is suggested to be the cause of some minor earthquakes, for instance the building of large reservoirs where the water stresses the surface rocks or the subsidence of deep mine workings.…

    • 2230 Words
    • 9 Pages
    Powerful Essays
  • Good Essays

    The Richter scale measures an earthquake based on the size of the seismic waves that it produces.…

    • 915 Words
    • 4 Pages
    Good Essays
  • Good Essays

    Earthquakes develop in the crust of the earth. The inner parts contains a lot of energy. Some of this energy can escape through cracks which can cause volcanic activity, but most of it is stored within the earth’s inner part, contained in the crust.The earth’s outer crust has rough edges and lines making it look a bit like a jigsaw puzzle.The energy stored here causes the pieces to slide, glide, knock and move around each piece. These pieces are also known as tectonic plates.…

    • 514 Words
    • 3 Pages
    Good Essays
  • Good Essays

    Below these plates is the mantle, a very hot section of the Earth where rocks are at the point of or is actually melting. These hot and molten rocks stream steadily making the plates above it move about. The plates move or rotate almost unnoticeably and at times collide against each other. Upon collision, the heavier plate slide beneath the lighter plate and is dipped against the hot mantle of the earth. This event is called subduction.…

    • 757 Words
    • 3 Pages
    Good Essays
  • Good Essays

    There are 5 different types of plate boundaries where the plates meet, move apart or rub along that provide processes and features that support continental drift and therefore plate tectonics. Volcanoes are a main feature at most plate boundaries as they come from magma chambers below the earths surface predominantly from melting plates. Other features include earthquakes, ocean trenches, mid ocean ridges and fold mountains. At all these different boundaries many processes occur at or around them. Firstly there is constructive this is where the two plates are moving apart this is normally in boundaries between two oceanic plates creating a lava upwelling from below, this causes oceanic ridges such as the mid Atlantic ridge, the two plates can be moving apart at either a slow, intermediate or rapid rate. Here not many processes take place a the plates are not colliding…

    • 1280 Words
    • 6 Pages
    Good Essays
  • Better Essays

    earthquake resistant design

    • 3106 Words
    • 13 Pages

    An earthquake (also known as a tremor, temblor or seismic activity) is the result of a sudden release of energy in the earth’s crust that creates SEISMIC WAVES. Earthquakes are measured with a seismometer; a device which also records is known as a seismograph.…

    • 3106 Words
    • 13 Pages
    Better Essays
  • Good Essays

    Earthquake Assignment

    • 395 Words
    • 2 Pages

    Have you ever got so mad you have to squeeze something to release your pressure? Or maybe you walk around aimlessly taking deep breaths to try and discharge the stress something or someone caused. Our earth, too, has a way of releasing pressure. Earthquakes are the result of the earth’s crust letting go of its strain and stress. Earthquakes can be defined as a sudden and violent shaking of the ground resulting when the earth’s crust releases pressure that has accumulated over time. Looking more into the study of plate tectonics can help to establish a better understanding of earthquakes.…

    • 395 Words
    • 2 Pages
    Good Essays
  • Powerful Essays

    An earthquake (also known as a quake, tremor or temblor) is the result of a sudden release of energy in the Earth's crust that creates seismic waves. The seismicity, seismism or seismic activity of an area refers to the frequency, type and size of earthquakes experienced over a period of time.…

    • 2028 Words
    • 9 Pages
    Powerful Essays
  • Powerful Essays

    An earthquake is caused by a sudden slip on a fault. The tectonic plates are always slowly moving, but they get stuck at their edges due to friction. When the stress on the edge overcomes the friction, there is an earthquake that releases energy in waves that travel through the earth's crust and cause the shaking that we feel.( readanddigest.com/what-is-an-earthquake)…

    • 1814 Words
    • 6 Pages
    Powerful Essays
  • Satisfactory Essays

    effects of earthquakes

    • 648 Words
    • 2 Pages

    Nature is a beautiful thing, and there is nothing in this world without nature. It gives many wonderful things to mankind. Although nature gives many things to mankind, sometimes it show its terrible side. It is obvious that most of disasters are very dangerous to anything in the world. Earthquakes are one of the terrible outcomes of nature, and they bring a lot of big problems to humans and the animals. An earthquake is an sudden and violent shaking of the ground because of released energy, and sometimes it causes great destruction and casualties. When it happens, everything that it crosses is destroyed. Therefore, there are three effects of earthquakes : tsunamis, volcanoes, and landslides.…

    • 648 Words
    • 2 Pages
    Satisfactory Essays
  • Good Essays

    ← An earthquake (also known as a quake, tremor or temblor) is the result of a sudden release of energy in the Earth's crust that creates seismic waves. The seismicity or seismic activity of an area refers to the frequency, type and size of earthquakes experienced over a period of time. Earthquakes are measured with a seismometer; a device which also records is known as a seismograph. The moment magnitude (or the related and mostly obsolete Richter magnitude) of an earthquake is conventionally reported, with magnitude 3 or lower earthquakes being mostly imperceptible and magnitude 7 causing serious damage over large areas. Intensity of shaking is measured on the modified Mercalli scale.…

    • 999 Words
    • 4 Pages
    Good Essays
  • Better Essays

    Earthquakes

    • 2019 Words
    • 9 Pages

    An earthquake is a shaking or trembling of the crust of the earth caused by underground volcanic action or by the breaking and shifting of rock beneath the surface. The volcanic action and shifting rocks create strain which continues to build to a sudden release of pressure resulting in a shock wave. The vibrations produced in the crust can vary from barely noticeable to enormously destructive. Shock waves can be classified into two broad categories. Waves that send particles oscillating back and forth in the same direction as the waves are traveling are called primary. Primary waves, sometimes called compressional waves, travel through the earth beneath the crust. Secondary waves cause vibrations which move perpendicular to the wave. These waves travel on the surface of the earth and move much slower than primary waves. Thus, when an earthquake occurs, seismic centers throughout the world record primary waves before the secondary waves arrive.…

    • 2019 Words
    • 9 Pages
    Better Essays