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Effects of earthquake Essay
Impacts of an earthquake
Earthquakes causes and effects
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I. Introduction to Earthquakes An earthquake is the shaking of the ground caused by sudden release of energy inside the earth's crust. It's the breaking and moving of tectonic plates along a fault line. Earthquakes can range in size from weak where we don't feel them to extremely violent where they actually thow people around and destroy cities. They may be a result of geological faults or other activites such as volcanoes, landslides, mine blasts and nuclear tests. An earthquake is not always naturally caused.
II. How Earthquakes happen Earthquakes are caused by tectonic plates moving in the earth's crust. They either move apart or pull together at faults. Two forms of faults are normal faulting where the hanging wall moves downward causing rocks to be pulled apart by tension and reverse faulting, which is the opposite where the hanging wall moves upward casuing rocks to be forced together by tension. These movements cause tectonic plate boundaries called divergent boundaries, convergent boundaries and transform boundaries. Each boundary is different and play a
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Primary impacts are the result of the ground shaking causing buildings to collaspe. This than results in the secondary impacts which are usually tsunamis, fires, landslides and other catastrophic events. Tsunamis, a huge wave of water, are one of the worse things human life can face after an earthquake as they are known to destroy absolutely everything in there path. Landslides, another huge destruction, is often known to be worse than the earthquake itself. These can cause whole cities to be completely destroyed as in Alaska, Turnagain Heights. Fires also cause a huge path of destruction. Broken gas lines set gas free making one little spark cause an inferno. An example of this would be the great earthquake of 1906 in San Fransisco which caused 90% fire damage among everything
Earthquakes are best described as a shaking or vibration of the ground caused by breaking of rock. Sometimes they are very strong and other times you would hardly notice them. This shaking occurs when stress that builds up in the crust is suddenly released as the crust breaks free and/or slides against the other pieces of crust. Earthquakes may also be thought of as the breaking of a popsicle stick by applying pressure to both ends at the same time. Should you try this experiment , you will feel the pressure build up as you apply more force until the stick snaps. When the stick snaps you will feel an instant of pain at your fingers as the stress reduces and energy waves move throughout the stick. When the earth's crust is placed under similar types of stress, binding as the stress builds, it will also snap and release the energy into the surrounding rocks, 'ooch'. Thinking about earthquakes will become more clear if you try another experiment.
Earthquakes play a major role into understanding the composition and materials that exist within the Earth (Merali and Skinner, 2009, p.252). Earthquakes are the main source of insight into the inner workings of the earth, due to the nature of the seismic waves they produce. P and S waves are reflected and refracted at different boundaries within the earth, and this enables seismologists to make inferences about the internal composition and structural of planet Earth. (Merali and Skinner, 2009, p.252).
Tsunamis caused by the Earthquake leads to flooding along the coastal environment. This damages any homes. Flooding caused new lakes or sag ponds on the land. Increasing groundwater flow from springs and displacing stream channel. ("Flood Consequences")
Earthquakes, by Webster’s dictionary definition, are, “a shaking or trembling of the earth that is volcanic or tectonic in origin.” World Book Encyclopedia reports scientists believe that more than 8,000 earthquakes occur each day without causing damage. A little more than 1,000 each year are strong enough to be felt. Earthquakes occur in the general sense, anywhere on land. Other earthquakes go by different names, such as volcanic eruptions and tsunamis, large tidal wave storms that occur underwater, primarily in the Pacific Ocean.
...tectonic movement of the plates, the stress forms along the fault and ultimately releases as an earthquake. On the pacific plate, Transform boundary along with the San Andreas fault. Transform-fault boundaries is when two plates that slide horizontally past another. Transform boundaries are usually found on ocean floor, but a few occur on the land. San Andreas fault zone is a transform fault, which connects East Pacific rise, in the south a divergent boundary, with South Gorda-Juan de Fuca-Explorer Ridge, yet another divergent boundary to the North. Ultimately because it’s a transform boundary, convergent boundary is strike-slipping past each of the plates in order to release pressure. As the San Andreas Fault is prime transform boundary between the North American Plate and the Pacific Plate, the Hayward Fault assumes a share of the total motion between the plates.
Before examining the Northridge event, understanding the naturally occurring hazard that is an earthquake will help to better understand exactly what happened and why it was such an important geological event. With four distinct layers, two layers, the crust and upper portion of the mantle, compose the skin that is the surface layer of the Earth. The crust is not a single, continuous piece. It is actually several different pieces, or plates, that come together to form the puzzle that comprises the surface of the Earth. These plates are in constant motion rubbing against one another. These areas, known as fault lines, where the plates rub up against one another have spots where one plate ”gets stuck while the rest of the plate keeps moving. When the plate has moved far enough, the edges unstick and is how most of the earthquakes around the world occur” (Wald, 2012). The energy stored from the friction of the two plate...
Where one is in the United States determines if one is in danger from a natural risk and which hazard. Some natural risks are earthquakes, tsunamis, volcanoes, hurricanes and tornadoes. Document one is a map from the natural Disaster Coalition that shows most natural risks and the areas affected in the United States. Despite showing specifically which regions are affected by certain natural risks, document one is not not complete and does not include all natural risks of the United States, leaving out certain ones like floods, wildfires, blizzards, landslides and numerous others. The west coast of the United States is prone to a lot of earthquakes. Earthquakes destroys infrastructures that leads to numerous deaths and a long recuperation periods.
This is because all of them move the crust in different ways. Weather it be a few tenths of degrees or multiple degrees, the plates are always moving. Sometimes when these plates collide, things like volcanoes can come to form. The boundaries can make things like: folded mountain ranges, volcanoes, earthquakes, trenches, mid ocean ridges, and rift valleys. Convergent boundaries are when the plates collide into each other.
The basic science is pretty straightforward. The earth lurches from time to time because its outer shell is broken into huge, solid plates floating on a layer of molten rock that has the consistency of Silly Putty. These tectonic plates are constantly jostling each other, like rafts crowded into a small pond, and its along the boundaries where they meet that most quakes are born.
There are many characteristics that make earthquakes along transform fault different from subduction zones, rift zones, and mid-ocean ridge transform faults. For instance, transforms faults are when two plates move past each other, shearing, with no creation or destruction of lithosphere. At transform faults, earthquakes are shallow and run as deep as 25 km. the magnitude of the earthquakes are smaller than 8.5 in the scale of Richter. In extensional boundaries, earthquakes are also shallow, but they occur only along the alignment of spreading and are smaller than 8 in magnitude. At compressional boundaries, earthquakes can be found at or near surface and at several hundred kilometers in depth.
They are the earth’s crust; they move very slowly every year. As the tectonic plates slide over each other they cause earthquakes. Earthquakes produce various damaging effects this includes damage to structures of buildings, bridges and other standing formations which then...
Plate tectonics can explain why there are earthquakes in the Earth reasonably. The definition of the earthquake is a fast and sudden movement of the Earth’s along geological faults, and the energy stored in stones is releasing in the meantime (Valentic, 2010). Figure 3 is showing some
Earthquakes are vibrations felt at the surface of the earth which are caused by disturbances of the energy in the earth's interior. These vibrations are known as seismic waves. (Skinner Robinson McVerry 1) There are different type sof seisimc waves such as Primary (P) waves, whcih travel the fastest, Secondary (S) waves which cause the earth to vibrate vertically, Surface (L) waves. P and S waves are "affected by changes in the density and the rigidity of the materials through which they pass." (Columbia Encyclopedia) Earthquakes vary in their intensity and duration. Often times they are strong enough to cause massive destriction. Tall buildings often suffer as a result of these natural disasters. In recent years this has become a larger and larger threat with both the number of large buildings, and their number of occupants increasing. In an effort to try to minimize the damage caused by earthquakes many some engineers focus primarily on designing and constructing earthquake resistant buildings. Earthquake engineers have gathered much of their information from analyzing past earthquakes, and learning which buildings can and can't withstand the tremors. The goals of these engineers is to design buildings that can withstand moderate earthquakes and obtain minimal damage, and that the buildings will not collapse lowering the probability of human deaths.
Earthquakes belong to the class of most disastrous natural hazards. They result in unexpected and tremendous earth movements. These movements results from dissemination of an enormous amount of intense energy in form of seismic waves which are detected by use of seismograms. The impact of earthquakes leaves behind several landmarks including: destruction of property, extensive disruption of services like sewer and water lines, loss of life, and causes instability in both economic and social components of the affected nation (Webcache 2).
Thousands of earthquakes happen every day around the world, but only a few of these are actually strong enough to be felt. And fewer still are strong enough to cause any damage to structures, even so Earthquakes have the ability to destroy entire cities or even entire countries (See 2011 Thoku Earthquake and Tsunami). But what causes earthquakes to occur, what happens to a cities infrastructure (Utilities, Roads, and Buildings) when one does strike, and what can city leaders and citizens do to prepare before one hits? There are three main causes of Tectonic Earthquakes. Tectonic because they are caused by the Tectonic Plates that the crust of the Earth’s surfaces rest on.