Earthquake Cause and Effect Essay Sample
Earthquakes are one of the worst and deadliest natural disasters that can occur. They are due to different factors and leave behind after-effects in their wake. An earthquake is the sudden release of strain energy in the crust of the planet’s surface, which will result in shaking that resonates outwards from the source. Simply, it is the sudden shaking of the Earth’s surface and can also be called a quake, tremor, or tremblor.
Earthquakes come in different sizes, as some are weak and cannot be felt, while others are violent and can destroy cities. The frequency, size, and type of quakes experienced are called seismicity. Earthquakes can be a result of volcanic action too. Furthermore, they have various effects that disturb lives and property.
The Valdivia Earthquake, also known as the Great Chilean, is the most powerful earthquake ever recorded. It occurred on the 22 nd of May, 1960, with studies placing it between 9.4 and 9.6 on the moment magnitude scale. The main cause of the quake was tension released by the Nazca plate under the South American plate. The earthquake lasted for about 10 minutes and resulted in tsunamis that affected Hawaii, southern Chile, eastern New Zealand, the Aleutian Islands, Japan, southeast Australia, and the Philippines.
Earthquakes are one of the most destructive and fascinating natural disasters that can cause a huge amount of destruction, injuries, and even death, but what makes them so dangerous? In this earthquake cause and effect essay sample, we will attempt to answer this question and explore why earthquakes occur and what effects they can have on society and the environment. Earthquakes are caused by sudden movement of the earth’s crust resulting from a release of energy from the Earth’s interior, and can be triggered by many different things including human activities such as mining and construction. Understanding the processes behind earthquakes can help individuals and organizations make better plans for future mitigation and adaptation if an earthquake were to occur. Additionally, students can buy a coursework to learn how to plan for an earthquake and develop better understanding of how to prepare for and cope with natural disasters.
Causes of Earthquakes
The main cause of the quakes is the sudden release of stress from the faults in the Earth’s crust. In this guide on how to do a cause and effect essay , we will cover the causes of an earthquake. As the continuous motion of layers transpires, it causes a gradual build-up of pressure on both sides of a fault. This happens because of plate boundaries that are moving. Once the stress is too significant, it is released in a shaky movement. So, how are earthquakes caused? Here are the factors causing quakes.
Tectonic Movements of the Earth
One of the leading causes of an earthquake is movement from the tectonics. This is a shift of the planes making up the crust. Our planet consists of about a dozen major plates and several minor ones and is constantly changing.
The tectonic plates frequently move slowly, but sometimes, they get stuck because of friction. When the stress on the crust becomes more significant than the friction, an earthquake happens to release energy. This brings about a shaky feeling in steps through the planet’s crust. Little movement from the tectonic caused big things such as the happenings in the Ring of Fire.
Seismicity Ripples
Seismic waves are one of the causes of earthquakes. These are elastic ripples generated by an impulse, like an earthquake. The energy from the fault in the crust of the planet will radiate outward in different directions through seismicity. Think of it as ripples on a pond. As the ripples move through the surface, they shake the floor and anything on it. These can be in the form of ripples, which is when an earthquake happens more than once. North Carolina earthquake events occur because of seismicity, although they don’t have significant damage.
Compressions in the Crust of the Earth
Compression in the crust happens when plate tectonics are pushed together. The crust will become shorter and thicker, and depending on how it reacts to the force, it can lead to an earthquake. Due to compression, many quakes that occur in Australia are caused by these shifts along faults. Also, the main cause of the Northridge earthquake 1994 was the compressions on the planet’s surface.
Volcanic Eruptions
Volcanic eruptions are one of the less likely causes of an earthquake, depending on the volcano that erupts. The earthquake will be triggered when an explosion of an explosive volcano. These ripples have a wider effect than volcanic eruptions when they trigger an earthquake. In the case of volcanic eruptions, around 20 miles of the region around the volcano will be affected when it erupts. The largest volcanic tremor took place under Mount St. Helens in 1981 , with an intensity of 5.5.
Disturbances on the Surface
In general, an earthquake can be caused by disturbances on the surface. Technology advancement is one of the popular cause/effect essay topics , which is to some extent responsible for catastrophes like an earthquake. Humanity builds skyscrapers, constructs dams, and gets water from underground. Dams and reservoirs are known to trigger earthquakes, especially when a dam structure fails.
For instance, the 2008 happening in Sichuan , China, which killed about 70,000 persons, was triggered by the nearby Zipping Dam construction. Another disturbance is groundwater extraction, as this can destabilize an existing fault. Hydraulic fracking is a method of extracting natural resources. It works when shale formations underneath are injected with a mixture of chemicals and water at high pressure. Fracking has had such an impact on the environment causing earthquakes.
Big buildings and skyscrapers can also add significant pressure on the Earth’s surface and crack rudimentary rocks.
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Effects of Earthquakes
When an earthquake happens, it leaves behind five primary outcomes and fires, a significant secondary impact of quakes. The effects of earthquakes on the Earth are often devastating, with people getting killed and injured, buildings getting destroyed, and the emotional and mental health of those affected. That’s why the investigation of this topic is so crucial in minimizing the adverse outcomes.
If you need an essay discussing this or any similar topic, our custom essay writing services can help you get the job done quickly and professionally. Now, let’s get to the main repercussions of quakes.
Ground Shaking
One of the most negative effects of earthquakes is surface shaking. During this time, buildings can be damaged, humans and animals will not be able to stand up or move around, and objects can be tossed around regardless of how big they are. Lives are taken in earthquakes but not directly by the shaking. Instead, it is caused by shaking, like buildings collapsing or getting hit by large objects.
The shaking of unstable slopes and direct blowout during an earthquake can lead to a landslide. Landslides are harmful effects of earthquakes and can damage buildings, tumbling hilltop homes, and block roads and transport lines. When a landslide happens, parts of the planet slide down and block an area. It can affect transportation after the earthquake, causing increased expenditure and leading to injuries and death for people there.
Surface Rupture
Another effect of quakes is surface breaking, which happens when the earthquake breaks the surface. As the earthquake occurs along a fault-line, it breaks through the Earth’s surface and can damage roads, pipelines, railway lines, tunnels, and airport runways. They will be damaged in the aftermath of an earthquake. An example of surface damage during an earthquake was the 1906 quake in California. The main cause of the quake was a slip of the San Andreas fault. The San Andreas fault is a major fracture of the planet’s crust.
Although this is a less common effect, an earthquake causes a tsunami. Tsunamis are water or tidal shakes that cause grave danger to places around the world, especially those in the Pacific Northwest region. An earthquake can cause the seafloor to move vertically apart from the normal floor. This will shake up the ocean and come in a series of floods to the beach. Tsunamis can move more than 700 kilometers per hour, causing flooding. It can damage properties and lead to death and injury too. Places close to the ocean are often subjected to tsunamis during an earthquake.
Liquefaction
Liquefaction is one of the outcomes of an earthquake that happens on the unconsolidated surface. When sediment grains are made to float in groundwater, the soil will lose all its solidity, and this is liquefaction. Tremors and earthquakes can cause mud and sand to spray over a couple of meters, posing a danger to buildings, train lines, gas lines, roads, and airport runways. Buildings can tip over and sink because of the liquefied soils, as occurred in the 1964 Niigata earthquake in Japan. Even septic tanks and gas tanks can float to the surface. Liquefaction after earthquakes leads to damages worth millions of dollars.
Earthquakes can have devastating consequences, so learning more about their causes and effects can be extremely beneficial. Recently, scientists have made tremendous progress in understanding the mechanisms behind earthquakes. To develop a deeper understanding of earthquakes, students may be required to write a coursework for me exploring the causes and effects of them. For example, they can focus on exploring tectonic plates and how they move and affect the ground, as well as the effect of natural conditions like weather and climate on their development. Additionally, the effects of an earthquake, such as structural damage and the resulting landslides, tsunamis and fires, can be further investigated in other science studies.
This essay has highlighted the cause and effect of earthquakes. Earthquakes are severe natural disasters caused by shifts in the crust of the Earth. Compressions on the planet’s surface, human disturbances like skyscrapers and dams, and tectonics moving can cause earthquakes. When they occur, consequences like landslides, ruptures, tsunamis, and more will follow. Some of the top countries prone to quakes are China, Indonesia, Turkey, Peru, Iran, Turkey, the United States, Japan, and Italy. China has gone through 157 earthquakes between 1900 and 2016. People living in these areas have precautions taken to protect themselves from injury during an earthquake.
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Earthquake and Its Devastating Effects
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What are the Effects of Earthquakes?
The effects from earthquakes include ground shaking, surface faulting, ground failure, and less commonly, tsunamis.
Ground Shaking
Ground shaking is a term used to describe the vibration of the ground during an earthquake. Ground shaking is caused by body waves and surface waves. As a generalization, the severity of ground shaking increases as magnitude increases and decreases as distance from the causative fault increases. Although the physics of seismic waves is complex, ground shaking can be explained in terms of body waves, compressional, or P, and shear, or S, and surface waves, Rayleigh and Love.
P waves propagate through the Earth with a speed of about 15,000 miles per hour and are the first waves to cause vibration of a building. S waves arrive next and cause a structure to vibrate from side to side. They are the most damaging waves, because buildings are more easily damaged from horizontal motion than from vertical motion. The P and S waves mainly cause high-frequency vibrations; whereas, Rayleigh waves and Love waves, which arrive last, mainly cause low-frequency vibrations. Body and surface waves cause the ground, and consequently a building, to vibrate in a complex manner. The objective of earthquake resistant design is to construct a building so that it can withstand the ground shaking caused by body and surface waves.
In land-use zoning and earthquake resistant design, knowledge of the amplitude, frequency composition, and the time duration of ground shaking is needed. These quantities can be determined from empirical (observed) data correlating them with the magnitude and the distribution of Modified Mercalli intensity of the earthquake, distance of the building from the causative fault, and the physical properties of the soil and rock underlying the building. The subjective numerical value of the Modified Mercalli Intensity Scale indicates the effects of ground shaking on man, buildings, and the surface of the Earth.
When a fault ruptures, seismic waves are propagated in all directions, causing the ground to vibrate at frequencies ranging from about 0.1 to 30 Hertz. Buildings vibrate as a consequence of the ground shaking; damage takes place if the building cannot withstand these vibrations. Compressional waves and shear waves mainly cause high-frequency (greater than 1 Hertz) vibrations which are more efficient than low-frequency waves in causing low buildings to vibrate. Rayleigh and Love waves mainly cause low-frequency vibrations which are more efficient than high-frequency waves in causing tall buildings to vibrate. Because amplitudes of low-frequency vibrations decay less rapidly than high-frequency vibrations as distance from the fault increases, tall buildings located at relatively great distances (60 miles) from a fault are sometimes damaged.
Taken from: Hays, W.W., ed., 1981, Facing Geologic and Hydrologic Hazards -- Earth Science Considerations: U.S. Geological Survey Professional Paper 1240B, 108 p.
Surface Faulting
Surface faulting is the differential movement of the two sides of a fracture at the Earth's surface and can be strike-slip, normal, and reverse (or thrust). Combinations of the strike-slip type and the other two types of faulting can be found. Although displacements of these kinds can result from landslides and other shallow processes, surface faulting, as the term is used here, applies to differential movements caused by deep-seated forces in the Earth, the slow movement of sedimentary deposits toward the Gulf of Mexico, and faulting associated with salt domes.
Death and injuries from surface faulting are very unlikely, but casualties can occur indirectly through fault damage to structures. Surface faulting, in the case of a strike-slip fault, generally affects a long narrow zone whose total area is small compared with the total area affected by ground shaking. Nevertheless, the damage to structures located in the fault zone can be very high, especially where the land use is intensive. A variety of structures have been damaged by surface faulting, including houses, apartments, commercial buildings, nursing homes, railroads, highways, tunnels, bridges, canals, storm drains, water wells, and water, gas, and sewer lines. Damage to these types of structures has ranged from minor to very severe. An example of severe damage occurred in 1952 when three railroad tunnels were so badly damaged by faulting that traffic on a major rail linking northern and southern California was stopped for 25 days despite an around-the-clock repair schedule.
The displacements, lengths, and widths of surface fault ruptures show a wide range. Fault displacements in the United States have ranged from a fraction of an inch to more than 20 feet of differential movement. As expected, the severity of potential damage increases as the size of the displacement increases. The lengths of the surface fault ruptures on land have ranged from less than 1 mile to more than 200 miles. Most fault displacement is confined to a narrow zone ranging from 6 to 1,000 feet in width, but separate subsidiary fault ruptures may occur 2 to 3 miles from the main fault. The area subject to disruption by surface faulting varies with the length and width of the rupture zone.
Taken from: Hays, W.W., ed., 1981, Facing Geologic and Hydrologic Hazards --Earth Science Considerations: U.S. Geological Survey Professional Paper 1240B, 108 p.
Ground Failure
Liquefaction Induced
Liquefaction is not a type of ground failure; it is a physical process that takes place during some earthquakes that may lead to ground failure. As a consequence of liquefaction, clay-free soil deposits, primarily sands and silts, temporarily lose strength and behave as viscous fluids rather than as solids. Liquefaction takes place when seismic shear waves pass through a saturated granular soil layer, distort its granular structure, and cause some of the void spaces to collapse. Disruptions to the soil generated by these collapses cause transfer of the ground-shaking load from grain-to-grain contacts in the soil layer to the pore water. This transfer of load increases pressure in the pore water, either causing drainage to occur or, if drainage is restricted, a sudden buildup of pore-water pressure. When the pore-water pressure rises to about the pressure caused by the weight of the column of soil, the granular soil layer behaves like a fluid rather than like a solid for a short period. In this condition, deformations can occur easily.
Liquefaction is restricted to certain geologic and hydrologic environments, mainly areas where sands and silts were deposited in the last 10,000 years and where ground water is within 30 feet of the surface. Generally, the younger and looser the sediment and the higher the water table, the more susceptible a soil is to liquefaction.
Liquefaction causes three types of ground failure: lateral spreads, flow failures, and loss of bearing strength. In addition, liquefaction enhances ground settlement and sometimes generates sand boils (fountains of water and sediment emanating from the pressurized liquefied zone). Sand boils can cause local flooding and the deposition or accumulation of silt.
Lateral Spreads - Lateral spreads involve the lateral movement of large blocks of soil as a result of liquefaction in a subsurface layer. Movement takes place in response to the ground shaking generated by an earthquake. Lateral spreads generally develop on gentle slopes, most commonly on those between 0.3 and 3 degrees. Horizontal movements on lateral spreads commonly are as much as 10 to 15 feet, but, where slopes are particularly favorable and the duration of ground shaking is long, lateral movement may be as much as 100 to 150 feet. Lateral spreads usually break up internally, forming numerous fissures and scarps.
Damage caused by lateral spreads is seldom catastrophic, but it is usually disruptive. For example, during the 1964 Prince William Sound, Alaska, earthquake, more than 200 bridges were damaged or destroyed by lateral spreading of flood-plain deposits toward river channels. These spreading deposits compressed bridges over the channels, buckled decks, thrust sedimentary beds over abutments, and shifted and tilted abutments and piers.
Lateral spreads are destructive particularly to pipelines. In 1906, a number of major pipeline breaks occurred in the city of San Francisco during the earthquake because of lateral spreading. Breaks of water mains hampered efforts to fight the fire that ignited during the earthquake. Thus, rather inconspicuous ground-failure displacements of less than 7 feet were largely responsible for the devastation to San Francisco in 1906.
Flow Failures
Flow failures, consisting of liquefied soil or blocks of intact material riding on a layer of liquefied soil, are the most catastrophic type of ground failure caused by liquefaction. These failures commonly move several tens of feet and, if geometric conditions permit, several tens of miles. Flows travel at velocities as great as many tens of miles per hour. Flow failures usually form in loose saturated sands or silts on slopes greater than 3 degrees.
Flow failures can originate either underwater or on land. Many of the largest and most damaging flow failures have taken place underwater in coastal areas. For example, submarine flow failures carried away large sections of port facilities at Seward, Whittier, and Valdez, Alaska, during the 1964 Prince William Sound earthquake. These flow failures, in turn, generated large sea waves that overran parts of the coastal area, causing additional damage and casualties. Flow failures on land have been catastrophic, especially in other countries. For example, the 1920 Kansu, China, earthquake induced several flow failures as much as 1 mile in length and breadth, killing an estimated 200,000 people.
Loss of Bearing Strength - When the soil supporting a building or some other structure liquefies and loses strength, large deformations can occur within the soil, allowing the structure to settle and tip. The most spectacular example of bearing-strength failures took place during the 1964 Niigata, Japan, earthquake. During that event, several four-story buildings of the Kwangishicho apartment complex tipped as much as 60 degrees. Most of the buildings were later jacked back into an upright position, underpinned with piles, and reused.
Soils that liquefied at Niigata typify the general subsurface geometry required for liquefaction-caused bearing failures: a layer of saturated, cohesionless soil (sand or silt) extending from near the ground surface to a depth of about the width of the building.
Taken from: Hays, W.W., ed., 1981, Facing Geologic and Hydrologic Hazards -- Earth Science Considerations: U.S. Geological Survey Professional Paper 1240B, 108 p.
Past experience has shown that several types of landslides take place in conjunction with earthquakes. The most abundant types of earthquake induced landslides are rock falls and slides of rock fragments that form on steep slopes. Shallow debris slides forming on steep slopes and soil and rock slumps and block slides forming on moderate to steep slopes also take place, but they are less abundant. Reactivation of dormant slumps or block slides by earthquakes is rare.
Large earthquake-induced rock avalanches, soil avalanches, and underwater landslides can be very destructive. Rock avalanches originate on over-steepened slopes in weak rocks. One of the most spectacular examples occurred during the 1970 Peruvian earthquake when a single rock avalanche killed more than 18,000 people; a similar, but less spectacular, failure in the 1959 Hebgen Lake, Montana, earthquake resulted in 26 deaths. Soil avalanches occur in some weakly cemented fine-grained materials, such as loess, that form steep stable slopes under non-seismic conditions. Many loess slopes failed during the New Madrid, Missouri, earthquakes of 1811-12. Underwater landslides commonly involve the margins of deltas where many port facilities are located. The failures at Seward, Alaska, during the 1964 earthquake are an example.
The size of the area affected by earthquake-induced landslides depends on the magnitude of the earthquake, its focal depth, the topography and geologic conditions near the causative fault, and the amplitude, frequency composition, and duration of ground shaking. In past earthquakes, landslides have been abundant in some areas having intensities of ground shaking as low as VI on the Modified Mercalli Intensity Scale.
Tsunamis are water waves that are caused by sudden vertical movement of a large area of the sea floor during an undersea earthquake. Tsunamis are often called tidal waves, but this term is a misnomer. Unlike regular ocean tides, tsunamis are not caused by the tidal action of the Moon and Sun. The height of a tsunami in the deep ocean is typically about 1 foot, but the distance between wave crests can be very long, more than 60 miles. The speed at which the tsunami travels decreases as water depth decreases. In the mid-Pacific, where the water depths reach 3 miles, tsunami speeds can be more than 430 miles per hour. As tsunamis reach shallow water around islands or on a continental shelf; the height of the waves increases many times, sometimes reaching as much as 80 feet. The great distance between wave crests prevents tsunamis from dissipating energy as a breaking surf; instead, tsunamis cause water levels to rise rapidly along coast lines.
Tsunamis and earthquake ground shaking differ in their destructive characteristics. Ground shaking causes destruction mainly in the vicinity of the causative fault, but tsunamis cause destruction both locally and at very distant locations from the area of tsunami generation.
143 Earthquake Essay Topics & Examples
Need a catchy title for an earthquake essay? Earthquakes can take place almost everywhere. That is why this problem is so exciting to focus on.
🏆 Best Earthquake Topic Ideas & Essay Examples
🎓 good essay topics on earthquake, 📌 catchy titles for earthquake essay, 👍 research titles about earthquake, ❓ essay questions about earthquake.
In your earthquake essay, you might want to compare and contrast various types of this natural disaster. Another option is to talk about your personal experience or discuss the causes and effects of earthquakes. In a more serious assignment like a thesis or a term paper, you can concentrate on earthquake engineering or disaster management issues. In this article, we’ve gathered best research titles about earthquake and added top earthquake essay examples for more inspiration!
- Crisis Management: Nissan Company and the 2011 Earthquake Expand on the points made in the case to identify the potential costs and benefits of these actions. The sharing of information was quite beneficial to Nissan in its response to the disaster.
- Natural Disasters: Tornadoes, Earthquakes, and Hurricanes Hence the loss may depend on the population of the area affected and also the capacity of the population to support or resist the disaster.
- Analysis of Damage to Apartment Buildings in the 1989 Loma Prieta Earthquake In turn, it is a prerequisite for the cataclysms in nature, such as earthquakes and the effect of liquefaction which was particular to the Marina district in the disaster of 1989.
- Mitigation of Earthquake Hazards The geologists should also inform the architects on the areas where earthquakes are likely to occur and how strong they will be able.
- Theory of Disaster: Earthquakes and Floods as Examples of Disasters The second category is that of those people who put their focus on the effects of the social vulnerability or the disasters to the society or to the people who are likely to be the […]
- Earthquakes Impact on Human Resource in Organizations The researcher seeks to determine the magnitude of this effect and its general effect on the society in general and the firms affected in specific.
- Natural Disasters: Earthquakes, Floods and Volcanic Eruption This is due to the relationship between an eruption and the geology of the area. It was observed that the mountain swelled and increased in size due to the upward force of magma.
- The Japan Earthquake and Tsunami of 2011 Documentary The documentary reflects the events leading to the natural disasters and their aftermath, including an investigation into the reasons for the failure of the precautionary measures in place during the 2011 earthquake in Japan.
- Natural Disasters: Earthquakes, Volcanoes, and Tsunamis In addition, the paper will outline some of the similarities and differences between tsunamis and floods. Similarities between tsunamis and floods: Both tsunamis and floods are natural disasters that cause destruction of properties and human […]
- Haiti Earthquake of 2010 Overview The purpose of this paper is to review the location and physical cause of the event, its human impact from it, and some of the interesting facts related to the disaster.
- Earthquake Prevention From Healthcare Perspective In terms of primary prevention of such a disaster, it is necessary to establish a public body or organization responsible for the creation of an extensive network of food, water, and first-aid kits to last […]
- Earthquakes in Chile and Haiti Moreover, the quake in Haiti raptured at the epicenter of the city with a high population density compared to Chile. Therefore despite a lower magnitude earthquake than Chile, Haiti suffered more damage due to the […]
- Earthquake Risk Reduction: Challenges and Strategies The victims of the earthquake in Haiti were hundreds of people, while the number of wounded and homeless was in the thousands. As for the latter, the worst scenario of the earthquake is created and […]
- Earthquakes and Their Devastating Consequences The break in the ground surface is the most common cause of horrific consequences, and people often cannot get out of the epicenter of the incident.
- Natural vs. Moral Evil: Earthquakes vs. Murder This problem demonstrates that such justifications for the problem of evil, such as the fact that suffering exists to improve the moral qualities of a person and thus serve the greater good, are unconvincing.
- Earthquake in South Africa: Reconstruction Process Therefore, it is vital for the government of South Africa to address the issues caused by the earthquake and reconstruct the region, focusing on several public interventions to stimulate the region’s growth in the shortest […]
- Earthquake in Haiti 2010: Nursing Interventions During natural disasters, such as the catastrophic earthquake in Haiti in 2010, nursing interventions aim to reduce the level of injury and provide the conditions for the fast recovery of its victims.
- Review of Earthquake Emergency Response The second resource is the supply of food and water that can help survivors wait for the rescue team for three days.
- California Earthquakes of the 20th Century Ultimately, the current essay examines the most devastating earthquakes in California in the 20th century and proposes a hypothesis of when the next large earthquake might strike.
- Human Activity and Growing Number of Earthquakes The pieces that support the opposing view claim that the data about their number may be distorted due to the lack of difference in the development mechanism of natural and artificial earthquakes.
- Researching the Earthquake Due to human activity, artificial earthquakes occur, and their number increases every year following the strengthening of destructive human impact on the planet.
- Disaster Preparedness and Nursing: A Scenario of an Earthquake In a scenario of an earthquake, nursing staff must be aware of the stages of disaster management and disaster preparedness in particular.
- Earthquake Disasters: Medical Response and Healthcare Challenges Therefore, an earthquake disaster infers abrupt and immense shaking of the ground for a duration and magnitude that can infringe the day-to-day activities. The last role of healthcare personnel in triage and intervention is to […]
- Wenchuan Earthquake: Impact on China’s Economy The earthquake made a moderate impact on the country’s economy, yet affected several industries located in the devastated areas.
- Recent Earthquakes and Safety Measures in California and Nevada The earthquake that is the largest by magnitude is in California. It is possible to minimize the damage by an earthquake.
- Role of the Nurses in the Site of the Haiti Earthquake The primary aim of the tertiary intervention conducted by the health practitioners was to reduce the effect of the diseases and injuries that occurred because of the Haiti earthquake.
- A Geological Disaster: Nisqually Earthquake in Washington State Geology refers to the study of the processes that lead to the formation of rocks and the processes that contribute to the shape of the earth.
- The Huaxian Earthquake: China’s Deadliest Disaster The main reason for the terrible earthquakes consequences was in the absence of a plan for the emergency case. After visiting China later in 1556, he wrote that the given disaster was likely to be […]
- The Sumatra Earthquake of 26 December 2004: Indonesia Tsunami As such, the earthquake resulted in the development of a large tsunami off the Sumatran Coast that led to destruction of large cities in Indonesia.
- Understanding Plate Tectonics and Earthquakes: Movements, Causes, and Measurement Therefore, the distance of the fracture will determine the intensity of the vibrations caused by the earthquake and the duration of the effect, that is, shaking the ground.
- Review of Public Meeting Regarded Earthquakes This focused meeting held in Port Au-Prince was to formulate the best strategies to help the people of Haiti anticipate, adapt and also recover from the impacts of earthquakes.
- Rebuilding Haiti: Post-Earthquake Recovery No doubt the tremors have taken a massive toll on the lives and resources of Haiti, but it was not only the tremors that caused the damage to such a massive extent.
- Earthquake Impacts: A Case Study of the 2010 Haiti Earthquake The short-term effects of the earthquake include food shortage, lack of clean water; breakdown of communication, lack of sufficient medical care, closure of ports and main roads, increased mortally, injuries, fires, the spread of communicable […]
- Public Awareness of Earthquake This will mean that the basement that is involved in thickening and shortening is mechanically required to produce the shape of zagros belt.
- Volcanoes: Volcanic Chains and Earthquakes The “Ring of Fire” is marked by the volcanic chains of Japan, Kamchatka, South Alaska and the Aleutian Islands, the Cascade Range of the United States and Canada, Central America, the Andes, New Zealand, Tonga, […]
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- Tōhoku Earthquake of 2011 The rate at which the pacific plate undergoes displacement is at eight to nine centimeter per annum, hence the plate subduction of the plate led to a discharge of large amounts of energy leading to […]
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- The 2011 Great East Japan Earthquake The earthquake was accompanied by a great tsunami given the high magnitude of the earthquake that reached 9. The third disaster was the meltdown of a number of nuclear plants following the tsunami.
- The 1979 Tangshan Earthquake The Tangshan Earthquake happened in 1976 is considered to be one of the large-scale earthquakes of the past century. The 1975 Haicheng Earthquake was the first marker of gradual and continuous intensification of tectonic activity […]
- The Parkfield Earthquake Prediction Experiment The seismic activity and the relatively regular sequence of the earthquakes in the area of San Paul Fault generated the interest of the geologists in exploring the processes in the rupture.
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- Losing the Ground: Where Do Most Earthquakes Take Place? Since, according to the above-mentioned information, natural earthquakes are most common in the places where the edges of tectonic plates meet, it is reasonable to suggest that earthquakes are most common in the countries that […]
- The Impacts of Japan’s Earthquake, Tsunami on the World Economy The future prospects in regard to the tsunami and the world economy will be presented and application of the lessons learnt during the catastrophe in future” tsunami occurrence” management.
- Geology Issue – Nature of Earthquakes Such an earthquake is caused by a combination of tectonic plate movement and movement of magma in the earth’s crust. Continental drift is the motion of the Earth’s tectonic plates relative to each other.
- The Great San Francisco Earthquake The length however depends on the size of the wave since the larger the wave the larger the area affected and consequently the longer the period of time taken.
- School Preparedness Plan for Tornado, Earthquakes, Fire Emergency In case of an earthquake emergency, the school should be prepared to keep the students safe. In case of a tornado emergency the school should be prepared to keep the students safe.
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- Why Did Haiti Suffer More Than Kobe as a Result of an Earthquake?
- Why Did the Earthquake in Haiti Happen?
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IvyPanda. (2024, February 26). 143 Earthquake Essay Topics & Examples. https://ivypanda.com/essays/topic/earthquake-essay-topics/
"143 Earthquake Essay Topics & Examples." IvyPanda , 26 Feb. 2024, ivypanda.com/essays/topic/earthquake-essay-topics/.
IvyPanda . (2024) '143 Earthquake Essay Topics & Examples'. 26 February.
IvyPanda . 2024. "143 Earthquake Essay Topics & Examples." February 26, 2024. https://ivypanda.com/essays/topic/earthquake-essay-topics/.
1. IvyPanda . "143 Earthquake Essay Topics & Examples." February 26, 2024. https://ivypanda.com/essays/topic/earthquake-essay-topics/.
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IvyPanda . "143 Earthquake Essay Topics & Examples." February 26, 2024. https://ivypanda.com/essays/topic/earthquake-essay-topics/.
Home / Essay Samples / Science / Earthquake / Earthquakes: Causes, Effects, and Implications
Earthquakes: Causes, Effects, and Implications
- Category: Science
- Topic: Earthquake
Pages: 1 (457 words)
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Introduction
Causes of earthquakes, effects of earthquakes, implications and preparedness.
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