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Earthquakes causes and effects
Impacts of an earthquake
Earthquakes causes and effects
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Earthquakes
What are earthquakes? An earthquake is what happens when two pieces of the earth suddenly slip past one another. The surface where they slip is called the fault or fault plane. The location below the earth’s surface where the earthquake starts is called the hypocenter, and the location directly above it on the surface of the earth is called the epicenter, or focus.
Sometimes, not always, an earthquake has foreshocks. These are smaller earthquakes that happen before the largest earthquake, or mainshock, in the same place. Scientists can’t tell that an earthquake is a foreshock until the mainshock happens. Mainshocks always have aftershocks that follow. These are smaller earthquakes that occur afterwards in the same place as the mainshock. Depending on the size of the mainshock, aftershocks can continue for weeks, months, and even years after the mainshock. The larger the mainshock, the larger the aftershocks will be.
What causes earthquakes and where do they happen?
The earth has four major layers: the inner core, outer core, mantle, and crust. The crust and the top of the mantle make up a thin skin on the surface of our planet. This skin isn’t all in one piece. It is made up of several pieces covering the surface of the earth, like a puzzle. These puzzle pieces keep slowly moving around, sliding past one another and bumping into each other. We call these puzzle pieces tectonic plates. The edges of tectonic plates are called plate boundaries. Plate boundaries are made up of many faults, and most of the earthquakes around the world occur on these faults. The edges of the plates are rough and get stuck while the rest of the plate keeps moving. Eventually the plate edges of a fault unstick and results in an earthquake.
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...or higher, the stronger and potentially more dangerous an earthquake is. Along with magnitude, intensity is observed as well. Intensity is the measure of force often acquainted with the shaking from the earthquake. Intensity varies on where you are located during the earthquake.
Unexpected Consequences of Earthquakes
Earthquakes commonly have consequences that are unexpected by an environment they occur in. The consequences may be tsunamis, buildings collapsing, structures distorting, landslides, and liquefaction.
Tsunamis
Works Cited
Harris, Tom, and Patrick J. Kiger. "How Earthquakes Work." HowStuffWorks. HowStuffWorks, Inc., 16 Jan. 2001. Web. 21 Apr. 2014. .
"The Science of Earthquakes." USGS. 24 July 2012. Web. 21 Apr. 2014. .
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 are a natural part of the Earth’s evolution. Scientific evidence leads many geologists to believe that all of the land on Earth was at one point in time connected. Because of plate tectonic movements or earthquakes, continental drift occurred separating the one massive piece of land in to the seven major continents today. Further evidence supports this theory, starting with the Mid-Atlantic ridge, a large mass of plate tectonics, which are increasing the size of the Atlantic Ocean while shrinking the Pacific. Some scientists believe that the major plate moveme...
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...
benchmark for the future, and integrated investigation into the effects of earthquakes in the U.S.
Earthquakes and volcanoes go hand in hand like peanut butter and jelly or rice and beans. Where there are volcanos there are usually tectonic plates beneath them either pushing against or pulling away from one another. Take for instance the Cascade Mountain Range in Northern California and stretches through Oregon and into Vancouver, British Columbia and sits northeast of the San Andreas Fault line that runs 750 miles through California. This fault creates the tectonic boundary between the Northern America and Pacific Plates. The three types of plate boundaries are convergent, meaning basically they are colliding together, divergent meaning they are pulling away from one another and transform which means that the plates slide past each other. During the convergence process some plates will subduct beneath the 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.
Earthquakes are common in both California and Japan and sometimes these areas are hit by large magnitude earthquakes that cause vast destruction. This is the case for both the 1994 Northridge Earthquake and the 1995 Great Hanshin-Awaji Earthquake (also commonly referred to as the Kobe Earthquake). Although both earthquakes were around a 6.0 magnitude and happened exactly one year apart from each other, they had very different impacts in terms of infrastructure, disruption of economy, health issues, and secondary hazards.
...sform boundary occurs where two plates slide against each other. But rather than sliding smoothly, the plates build up tension, then release the tension with a spurt of movement. This movement is felt as an earthquake. The San Andreas fault system is the most famous example of this type of boundary. Here two plates move laterally past each other and oceanic crust is neither created nor destroyed. A collisional boundary occurs where two land masses on plates are pushed together. Trying to occupy the same space, the land masses buckle and fold, creating mountain ranges. In conclusion there are four types of plates. They are constantly moving because of the convection cell. Because of the plate colliding the earth changes in shape. By Earthquakes, Mountains and hills, the earth will continue to move as long as these plates are around; and they aren't going anywhere.
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 result in injuries and people getting killed, wildlife getting disrupted as well as humans. An earthquake can affect the earth as it’s easier to let the lava come out of the earth. Tsunamis- Can cause financial problems such as home loss, job loss which will then result in being homeless, loss of crops and food supplies which causes a lot of harm to us ‘humans’. A tsunami is a series of waves that send surges of water that can travel thousands of miles.
Earthquakes are sudden, violent shakings in the ground that is caused by the movement of the Earth’s crust or volcanoes. More than 10,000 earthquakes take place every year, most of them not recognized by humans. Earthquakes do not occur at random locations, however, as some people believe. A pattern can be seen where most earthquakes occur at or near the plate boundaries. In fact, these earthquakes are what help scientists discover where these plate boundaries are. Plate boundaries are the cracks between the set of tectonic plates that make up the Earth’s crust. The moving of these tectonic plates is what causes these earthquakes. There are three types of plate boundaries: divergent boundaries, convergent boundaries, and transform boundaries.
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).
The crust, the outermost layer of the earth, which compares to the shell or skin. The earth kind of looks like a big jawbreaker because it has so many layers. Tectonic plates move in a constant motion, driving them into one another. The plates will meet at a fault. One plate pushes against another one and creates friction, which holds the plates together at the fault line, the rest of the plate remains in motion. Once the pressure grows so strong, the plates slip and release all the built up energy in the form of seismic waves in all directions. The seismic waves travel through the earth making it shake. When they reach the surface, they shake everything else like houses and people (Lisa Wald, 2009). Locating earthquakes is the important key to keeping people