cause and effect essay on earthquakes

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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Over the centuries, earthquakes have been responsible for millions of deaths and an incalculable amount of damage to property. Depending on their intensity, earthquakes (specifically, the degree to which they cause the ground’s surface to shake) can topple buildings and bridges , rupture gas pipelines and other infrastructure, and trigger landslides , tsunamis , and volcanoes .  These phenomena are primarily responsible for deaths and injuries. Very great earthquakes occur on average about once per year.

Earthquake waves, more commonly known as seismic waves , are vibrations generated by an earthquake and propagated within Earth or along its surface. There are four principal types of elastic waves: two, primary and secondary waves, travel within Earth, whereas the other two, Rayleigh and Love waves, called surface waves, travel along its surface. In addition, seismic waves can be produced artificially by explosions.

Magnitude is a measure of the amplitude (height) of the seismic waves an earthquake’s source produces as recorded by seismographs . Seismologist Charles F. Richter created an earthquake magnitude scale using the logarithm of the largest seismic wave’s amplitude to base 10. Richter’s scale was originally for measuring the magnitude of earthquakes from magnitudes 3 to 7, limiting its usefulness. Today the moment magnitude scale, a closer measure of an earthquake’s total energy release, is preferred.

Earthquakes can occur anywhere, but they occur mainly along fault lines (planar or curved fractures in the rocks of Earth’s crust ), where compressional or tensional forces move rocks on opposite sides of a fracture. Faults extend from a few centimetres to many hundreds of kilometres. In addition, most of the world’s earthquakes occur within the Ring of Fire , a long horseshoe-shaped belt of earthquake epicentres , volcanoes , and tectonic plate boundaries fringing the Pacific basin .

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earthquake , any sudden shaking of the ground caused by the passage of seismic waves through Earth ’s rocks. Seismic waves are produced when some form of energy stored in Earth’s crust is suddenly released, usually when masses of rock straining against one another suddenly fracture and “slip.” Earthquakes occur most often along geologic faults , narrow zones where rock masses move in relation to one another. The major fault lines of the world are located at the fringes of the huge tectonic plates that make up Earth’s crust. ( See the table of major earthquakes.)

Little was understood about earthquakes until the emergence of seismology at the beginning of the 20th century. Seismology , which involves the scientific study of all aspects of earthquakes, has yielded answers to such long-standing questions as why and how earthquakes occur.

About 50,000 earthquakes large enough to be noticed without the aid of instruments occur annually over the entire Earth. Of these, approximately 100 are of sufficient size to produce substantial damage if their centres are near areas of habitation. Very great earthquakes occur on average about once per year. Over the centuries they have been responsible for millions of deaths and an incalculable amount of damage to property.

The nature of earthquakes

Causes of earthquakes.

Earth’s major earthquakes occur mainly in belts coinciding with the margins of tectonic plates. This has long been apparent from early catalogs of felt earthquakes and is even more readily discernible in modern seismicity maps, which show instrumentally determined epicentres. The most important earthquake belt is the Circum-Pacific Belt , which affects many populated coastal regions around the Pacific Ocean —for example, those of New Zealand , New Guinea , Japan , the Aleutian Islands , Alaska , and the western coasts of North and South America . It is estimated that 80 percent of the energy presently released in earthquakes comes from those whose epicentres are in this belt. The seismic activity is by no means uniform throughout the belt, and there are a number of branches at various points. Because at many places the Circum-Pacific Belt is associated with volcanic activity , it has been popularly dubbed the “Pacific Ring of Fire .”

A second belt, known as the Alpide Belt , passes through the Mediterranean region eastward through Asia and joins the Circum-Pacific Belt in the East Indies . The energy released in earthquakes from this belt is about 15 percent of the world total. There also are striking connected belts of seismic activity, mainly along oceanic ridges —including those in the Arctic Ocean , the Atlantic Ocean , and the western Indian Ocean —and along the rift valleys of East Africa . This global seismicity distribution is best understood in terms of its plate tectonic setting .

Natural forces

Earthquakes are caused by the sudden release of energy within some limited region of the rocks of the Earth . The energy can be released by elastic strain , gravity, chemical reactions, or even the motion of massive bodies. Of all these the release of elastic strain is the most important cause, because this form of energy is the only kind that can be stored in sufficient quantity in the Earth to produce major disturbances. Earthquakes associated with this type of energy release are called tectonic earthquakes.

Essay on Earthquake | Types, Causes & Effects

The earthquake is one of the worst experiences that can shake the earth up and down, leaving death and destruction all around. Read complete essay on earth definition, types, causes & effects, prevention, etc with examples

Table of Contents

Essay on Earthquake, Types, Causes & Effects

An earthquake is a natural calamity caused by the movement of tectonic plates present under the surface of the earth. The movement of tectonic plates causes damage and destruction, earthquake is often named a destructive phase of nature. The magnitude of the earthquakes is measured on the Richter scale.

This is one of the most damaging natural calamities which is hardly detected by seismologists, the branch of science called seismology is purely dedicated to the study of earthquakes, many advancements have been made to determine the sudden occurrence of this natural calamity.

However hard scientists try but they have greatly failed to determine the exact time and date of this natural calamity. The forecasting and prediction regarding this natural calamity hardly benefit humans. Scientists have stated that all volcanic regions are more prone to earthquakes as compared to other religions, volcanoes cause frequent earthquakes.

The movement of magma and volcanic eruptions shake earth which brings movement in tectonic plates and earthquake occurs. Volcanic earthquakes cause more destruction. Japan is the most prone country to earthquakes, it is highly affected by this natural calamity.

Causes of Earthquake

The main causes of earthquakes are volcanic eruptions, geographical faults, and human activities. Human activities like nuclear bombing and mining are major causes of earthquakes. The displacement of plates from their original position cause earthquakes. The breaking of the rocks underneath the surface of the earth cause earthquakes.

Effects of Earthquakes

Earthquakes cause loss of lives, destroy buildings and plazas, violent earthquakes cause mass destruction. Since time immemorial our planet earth has been hit by several small and violent earthquakes which not only damaged properties, buildings, and houses but also many innocent lives were lost.

Earthquake in a sea bed causes tsunami which causes huge loss of lives. The ground rupture due to earthquakes is harmful to dams, bridges, and nuclear power stations. When it is measured higher on the Richter scale it causes fires in forests, rubbing of trees produces fire which is very damaging.

Earthquake is natural, sometimes it causes no damage, it proves very little devastating when it is mild and at a small scale. Even if it is small, the slightest tremors spread panic and fear among people.

Precautions/Prevention

• Evacuate houses, homes, offices schools, buildings and run to open areas when it occurs or is warned.
• Don’t stand near to any collapsing building or any falling object.
• If don’t find time or place to run hide under any table or bed.
• Carry all necessary like food, water, medicines, documents, credit cards, debit cards, or cash in a bag in case of emergency.

Earthquake is one of the greatest natural calamities of the world, it has caused the loss of thousands of lives and has made humans suffer a lot.

Annually many earthquakes occur throughout the world which is potentially very dangerous. None can stop this calamity to occur but we can only wisely act to save our lives and loss of property.

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What Happens During an Earthquake?

What causes earthquakes, and what types of earthquakes are there? To answer these questions, it is first helpful to have an understanding of Earth’s composition.

Earth basics

Earth is made up of

• a solid inner core
• a molten outer core
• the thick and mostly solid mantle, which occupies approximately 84 percent of the earth's total volume
• the comparatively thin crust, which varies between 5 to 50 km in thickness.

Earth's outer skin is not a continuous surface. Instead, it is composed of massive segments called tectonic plates . Earthquakes occur along the boundaries between tectonic plates or at the site of cracks within the plates, which are called faults .

What causes earthquakes?

The tectonic plates that make up the earth's crust are moving constantly. As the edges of these plates slide against each other in fault zones, friction can slow them down, leading to the buildup of pressure over long periods of time. When the force of movement finally overcomes the friction, sections of the crust suddenly break or become displaced, releasing the pent-up pressure in the form of seismic waves. This is a naturally occurring earthquake, sometimes referred to as a tectonic earthquake .

While tectonic earthquakes can occur at any location around the world, the majority of large earthquakes—about 80 percent—occur at the circum-Pacific seismic belt found along the rim of the Pacific Ocean. Two other regions regularly exhibiting earthquakes include the Alpide belt, extending along the southern margin of Eurasia through the Himalayan Mountains, Sumatra, and Java; and the Mid-Atlantic Ridge running along the floor of the Atlantic Ocean.

When an earthquake occurs, different types of energy waves are generated.

• "P waves" or "primary waves" are the first waves to be detected. These are compressional waves that push and pull as they move through rock and fluids.
• "S waves" or "secondary waves" are the next waves to be detected. These waves move only through rock. They move up and down or side to side, perpendicular to the direction in which the wave is moving.
• Surface waves follow P and S waves. They travel along the surface of the earth and thus cause the most damage. Surface waves can be characterized as Love waves, which are faster and move the ground from side to side, and Rayleigh waves, which roll like waves on the surface of oceans and lakes.

What other types of earthquakes exist?

In addition to tectonic earthquakes, seismologists have classified three more earthquake types:

• Volcanic : Earthquakes that occur in conjunction with volcanic activity
• Collapse: Smaller-scale earthquakes that result from the subterranean collapse of caverns or mines
• Explosion: Earthquakes caused by underground explosions of nuclear or chemical devices.

Does fracking cause earthquakes?

"Fracking" is an informal term for hydraulic fracturing, a process used to increase the flow of oil or gas to a production well. It involves the injection of large volumes of water, sand, and chemicals under high pressure into a bedrock formation to create new fractures in the rock or increase the size, extent, and connectivity of existing fractures, leading to more permeability.

On rare occasions, fracking can lead directly to earthquakes . More frequently, earthquakes are induced by the disposal of waste water associated with the oil production into underground wells. Seismic events associated with fracking and waste fluid disposal tend to be low-level and dependent on conditions such as the injection rate and total volume injected, the proximity of faults near the injection site and the pathways permitting pressure to travel from the injection site to the fault, and the presence of stresses on faults that are large enough to produce earthquakes.

Dive Deeper

ENCYCLOPEDIC ENTRY

Earthquakes.

Earthquakes happen everyday around the world. Often, people can’t feel them, but sometimes they cause great devastation.

Earth Science, Geology

Woman Awaiting Aid after Earthquake

While most earthquakes are barely noticeable, others can be devastating. Major earthquakes—magnitude 7.0-7.9—and great earthquakes—magnitude of 8.0 or higher—can destroy buildings and kill people and other animals.

Photograph by ARKO DATTA/AFP

Hundreds of earthquakes occur on Earth everyday. Most of them are small, barely detectable by most people. But occasionally there is a much more significant quake. On average, a major earthquake —one with a magnitude of 7.0-7.9—strikes somewhere on the planet more than once a month. A great earthquake —with a magnitude of 8.0 or higher—occurs about once a year. An earthquake can happen anywhere. However, the vast majority of earthquakes occur at the boundaries between tectonic plates . Continental and oceanic plates may move toward each other, scrape past each other, or pull apart as they move slowly across the planet's upper mantle. This movement of the plates, and the pressure that is built up at the boundaries, can result in earthquakes . The boundaries between plates contains systems of deep cracks, called faults . Most earthquakes occur along these faults . Within a fault , rock masses on either side of the break are pushed by geologic forces in opposite directions. Friction , however, holds the rocks in place, causing stresses to build. Finally, the mounting pressure overcomes the friction and a sudden movement occurs along the fault , releasing a large amount of energy. This is an earthquake . While the vast majority of earthquakes occur along faults at Earth's plate boundaries, occasionally, a quake occurs in the middle of a plate, far from any boundary. Such quakes make up less than 10 percent of all earthquakes . While these intraplate quakes are not completely understood, scientists theorize that they may result from weaknesses within Earth’s crust from long ago. Although rare and not well understood, these earthquakes are no less devastating than those that occur along plate boundaries. Earthquakes along the New Madrid Fault , along the Mississippi River in the United States, in 1811–1812 were among the strongest quakes ever recorded. More recently, in 2001, an intraplate earthquake in the Gujarat region of northwesternn India killed more than 20,000 people. Believe it or not, earthquakes aren’t just Earth-bound phenomena. Astronauts who traveled to the moon in the late 1960s and early 1970s installed seismographs , devices used to measure and record vibrations, on the lunar surface. The data radioed back to Earth showed that “moonquakes” occur and can be fairly strong and last much longer than quakes on Earth!

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Earthquakes: Causes, Effects, and Implications

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Causes of earthquakes, effects of earthquakes, implications and preparedness.

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