The Valdivia Earthquake: One of the Most Powerful in History

The Valdivia Earthquake
Earthquakes, also referred to as temblors, are one of the world's most powerful occurrences. The Earth has four layers: the crust, mantle, inner and
outer core. Earthquakes occur in the crust and upper mantle (Refer to Figure 1). The mantle is made up of semi–molten rock called magma. The upper
mantle rock is hard. The crust is the outer layer of the earth. Together, the crust and upper mantle make up thelithosphere. The lithosphere is 20–50 km
thick and is cracked. The asthenosphere sits below the lithosphere. The lithosphere consists of tectonic plates (lithospheric plates). Tectonic plates is the
theory that the Earth's outer shell is divided by slabs of solid rock. When these two tectonic plates make frictional contact the outcome may be deadly.
Sometimes there can be smaller shocks that occur, one's before called the foreshock, and one's after called the aftershock and the main earthquake called
the main shock.
The richter scale, developed ... Show more content on Helpwriting.net ...
Megathrust earthquakes are the most powerful earthquakes in the world and can produce tsunamis through a variety of structures. The Valdivia
earthquake, in theory, is a convergent the earthquake was caused by the Nazca plate releasing tension and descending underneath the South American
Plate.The Great Alaska earthquake also appears to be a convergent boundary earthquake as the Pacific Plate lurched underneath the North American
Plate causing the earthquake.
Seismic waves are waves of energy that travel through the Earth's layers as a result of earthquakes. During an earthquake, the waves released may be
"P" or "S" depending on the way and speed of the wave (Refer to Figure 3 and 4). P–waves, or primary waves are longitudinal waves. Their vibrations
are along the same direction as the direction of travel. P–waves are faster than S–waves. S–waves, or secondary waves are transverse waves. They
travel at right angles to the direction of
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The Northridge Earthquake
Knowledge is the skill acquired by a person to have facts or information through education or experience. To wonder is to be curious to know something.
The meaning behind Morgan's quote is that once someone learns something new, they want to investigate or know more.
Once we are told something we did not know, our curiosity tells us to do some research or to ask questions in order to know more about the topic. I
have been in this situation multiple times. When I was first told about the Northridge Earthquake that happened a few years ago, I was shocked and I
was dying to know more. I had to do some research on my own and my knowledge about the earthquake expanded. Not only did I know what
happened, but I also knew how it happened, why it

The Vancouver Earthquake
destruction, as a result of movements within the earth's crust of volcanic action. Well no parts of the surface of the earth are protected from
earthquakes, but some parts of the world experience earthquakes more frequently than others do. You will find that earthquakes are usually most
common at tectonic plate boundaries where different plates meet. The largest events usually happen where two plates are colliding or colliding and
sliding past one another, particular around the edge of the pacific plate. Large shallow earthquakes also happen where two plates are pulling apart with
the creation of new oceanic crust along mid–ocean ridges and on the transform faults that intersect them. Shallow intraplate earthquakes occur in the
relatively stable interior of continents away from... Show more content on Helpwriting.net ...
The time of this disaster was from the 22 of February 2011 at 12:51pm. The earthquake hit the Canterbury region in New Zealand's south island and
was centered 2 km west of the port town of Lyttelton, and 10km south east of the center of Christchurch, at the time ne Zealand's second most
populous city. The damages to Christchurch where shocking as there were road and bridge damage and hampered rescue efforts. Soil liquefaction
and surface flooding also occurred. Road surfaces were forced up by liquefaction, and water and sand were spewing out of cracks. A number of cars
were crushed by falling debris. In the central city, falling buildings crushed two buses. Because the earthquake hit during the lunch hour, collapsed
buildings buried some people on the footpaths. Damage also occurred to many older buildings and on the 28th of February 2001 the prime minster at
the time announced that there would be an inquiry into the collapse of buildings that had been signed off as sale after the 4 September 2010
earthquake, This earthquake killed an amount of 180 people which is shown on page 2 and this is

Wind, Earthquake And Its Effect On The Earthquake Essay
Unlike wind, earthquake is a different phenomenon which generates a ground motion. The intensity or acceleration of the earthquake depends upon
the magnitude and location of its epicenter. The seismic waves caused by the earthquake cause inertial forces in the building. The inertial forces are
created when an outside force tries to move a body in rest which happens in this case as seismic waves tries the move the building in rest. We all know
that when a building is subjected to inertial forces it should obey the newton's second law of motion.
F=M.a –––––––––––––––––––– (3)
Where 'F' is inertial force and 'M' denotes mass of building and 'a' is the acceleration with which the building is moved due to seismic activity.
Duration, velocity and displacement:
From the newton's second law, it is evident that acceleration is a key factor in determining the forces on a building. But there is one more criteria that
we have to look into is the duration of the earthquake. Earthquake that has moderate acceleration, sustained over time, can cause much more damage to
buildings than a single much larger peak. It weakens the building structure and reduces its durability. The strong–motion duration is often termed as
"bracketed duration" (Arnold 2013). This is the shaking duration above a certain threshold acceleration value, which is 0.05g, and is defined as the
time between the first and last peaks of motion that exceeds this threshold value (Arnold 2013). The strong motion

Earthquake : The Seddon Earthquake
In Seddon the aftershocks were a lot fewer but there were still 1,700 and only 45 being over magnitude 4. (see image 2). From the earthquake features
discussed, we can see that despite the Seddon earthquake having a greater magnitude and similar type of fault movement, it was the fact that the
Christchurch earthquake carried a lot more power and force with its initial ground movement and shaking, and its continual aftershocks, that the effects
of this earthquake were much worse than the Seddon earthquake.
In Christchurch, after the earthquake, more than half of the buildings in the central business district, around 10,000, had to be demolished, with a
total of 100,000 homes damaged. Many heritage buildings were also badly damaged and some had to be demolished, with the most recognisable the
Christchurch Cathedral. This damage in Christchurch was especially bad due to the effect of seismic lensing. Seismic lensing is caused during an
earthquake when the p, s and I waves produced by the earthquake bounce of their surroundings. If these surroundings have hard surfaces the waves
will rebound back in a similar direction to where they came from. Whereas if the surfaces properties are softer they can be

The Great Chilean Earthquake : An Earthquake
The Great Chilean Earthquake An earthquake is the shaking of the earth by seismic waves radiating away from the disturbance, most commonly fault
movement. The great Chilean earthquakes origin was of the coast of Chile at a subduction zone, referred to as a hot spot for seismic activity. A
subduction zone is a region on the crust of the earth where two tectonics plate meet one another. The area where the two plates meet is called a plate
boundary. When two plates meet at a subduction zone, they converge towards each other, and one these tectonic plates come into contact with each
other, one bends and slides underneath another, resulting in one curving down to the mantle. In this circumstance when subduction is taking place the
denser plate is the one that sinks beneath the other. On the earth's surface there are two main types of crust; the oceanic and the continental. The
continental isn't as dense as the oceanic making it slide above while the oceanic subducts down, in a convection motion to recycle itself then be
remade when it pushes itself up. The place the denser medium goes towards is the mantle that consists of molten rock and it accounts to 84% of earths
volume. Subduction only takes effect when two plates of different density collide, for if two continental crusts converge and push together neither will
subduct, so it will be like a car crash where the two mediums smash into each other but neither subducts, as an example of this event look to the
Himalayas that were

An Earthquake Of The Francisco Earthquake
Giovanni Lozano
Professor Tod Benedict
GLY 1000
21 October 2015
1906 San Francisco Earthquake An earthquake is the vibration of the Earth produced by the rapid release of energy. Most earthquakes occur at a plate
boundary, usually along the Circum–Pacific belt. They tend to be caused by the slippage along large fracture in the Earth's crust, such as a fault for
example. However, they can also occur from a volcanic eruption, or an atomic explosion. There are two different types of shocks to a major earthquake;
there is a foreshock and an aftershock. The foreshock concedes of smaller earthquakes that precede a major one by some time period, and an
aftershock that concedes of small earthquakes due to the adjustment of the crust after the major earthquake. Earthquakes affect numerous things, from
soil liquefaction to construction, and the rupture of power, gas, and water lines. There are two ways to measuring the size of an earthquake, those are
intensity and magnitude. The intensity is a measure of the degree of an earthquake shaking at a given locale based on the amount of damage,
measured through the Modified Mercalli Intensity Scale which bases of the surveys of those whom were affected, and ranges from 1 to a 12. The
magnitude is the total amount of energy released at the source of an earthquake, which tends to be measured on the Richter magnitude scale. This
method is based on the amplitude of the largest seismic wave, and ranges from a –2 to infinity. Unfortunately there

Earthquake Of The Sichuan Earthquake
The Sichuan Earthquake also known as Wenchuan Earthquake occurred on May 12th, 2008. The horrific earthquake was located in the mountainous
dominant region of Sichuan, south–western China. The earthquake was measured to have a magnitude of 8.0 by the Chinese. The quake affected
four–fifths of the buildings located in the area. Towns, villages and schools had collapsed and had been destroyed. Close to 90,000 people were
tallied as missing or dead. The Chinese Government report stated that more than 5,300 Children (mainly students at school) were killed by the quake.
As well as 375,000 people injured from collapsing buildings and tumbling debris. The Chinese government sent relief workers and 130,000 soldiers to
the devastated location. Yet remote villages were hard to reach due to the insignificant amount of usable rescue equipment needed to clear the damage
(Pletcher, n.d.). 4,800,000 people (BBC, 2013) were left homeless due to the earthquake.
The prediction of earthquakes cannot be tallied as a certain thing at the present time, however educated estimations can be used to develop and warn
people of possible earthquakes. Predictions can and are based on a few factors. One includes new cracks in rocks, this occurs due to a great build–up of
energy. That could possibly lead to a site where a discharge of energy could take in the nearby future. Seismic danger maps arranged on the basis of
historic earthquake accounts and estimates of earthquake movement in the destination

On Earthquakes Essay
On Earthquakes
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 ... Show more content on Helpwriting.net ...
The modern seismograph was invented early this century by a Russian seismologist, Prince Boris Golitzyn. This device made possible the modern era of
earthquake research.
Although earthquakes have occurred and affected mankind for as long as humans have been around, historical records are either lacking or
considered unreliable before the middle of the 18th century. However, some records do exist and date major earthquake events back to 425 BC when
one occurred off the coast of Greece resulting in an island named Euboea. Another occurred in Asia Minor about AD 17 and another leveled much of
the Roman city of Pompeii in AD 63. During the Middle Ages, severe earthquakes struck England, in 1318; Naples, Italy, in 1456; and Lisbon,
Portugal, in 1531.
Casualties from major earthquakes have resulted in the greatest disasters in history. The worst occurred in 1556 in the Shannxi (Shensi) Province in
China and killed an estimated 800,000 people. During the 18th century, the Japanese city of Edo (site of modern day Tokyo) was struck and killed
200,000. Earthquakes in Sicily in 1693 and Lisbon in 1755 each killed about 60,000 people. In 1797, approximately 40,000 died when Quito, Ecuador
was struck.
Historically, the most powerful earthquakes to strike North America occurred in 1811 and 1812 in southeastern Missouri. However, the most famous
earthquake to strike in North America

How Does Earthquake Affect The Earthquake
Task Two: Earthquakes and Buildings
The type of buildings that were the most damaged in the 2011 Christchurch earthquake.
In the 6.3 magnitude Christchurch earthquake that occurred at 12.51pm on the 22nd of February 2011, the types of buildings that were the most
damaged were houses and commercial buildings that were built in the 19th and early 20th century. The majority of these buildings that were damaged
were ones that relied on single or double brick for their structure. This relates to how the bricks are placed on the house and whether there are two
layers or one layer of brick. Buildings made of bricks and stones were damaged because they can't move with the earth and most of the bricks crack
and fall off making the structure a lot less stable and more likely to collapse in an aftershock.
Brick chimneys on the old wooden houses fell over and crashed through the roofs and caused a lot of damage. Stone buildings such as the Old Stone
House were also badly damaged and had to be closed following the February 2011 earthquake. The most structural damage mainly occurred in houses
that were made of heavy materials such as stones, bricks or concrete. This is because it is harder for these building materials to withstand strong
shaking and to support their own weight when they begin to lose shape. They can't bounce back as easy once they have been forced in the other
direction. This forces the buildings to fall outwards or collapse.
A lot of damage occurred in houses and

Pompei Earthquake
A good thing to study is how earthquakes work,and the impact of the earthquake of pompeii. The location where it occurred at is a part of Italy, in
Italy Pompeii,and Mount Vesuvius(See appendix A map for visual location). Sixteen years after the tell tall in 79AD, Mount Vesuvius erupted again. A
seismometers was used to measure the magnitude of the earthquake of Pompeii that caused the eruption of Mount Vesuvius. The topics that will be
studied are, what is an earthquake, what causes an earthquake,impact of what earthquakes have on the world, and Pompeii today and earthquakes today.
An earthquake is what happens when two blocks of the earth suddenly slip past one another. The surface where they slip is called the fault of 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. There are four types of earthquakes tectonic,volcanic,collapse,and explosion. Another good topic to study is deeper into
the science of earthquakes. "Most earthquakes occur along faults, or breaks, in the Earth's crust." by Bill Haneberg.http://tremor.nmt.edu/faq/what.html
The main reason why an earthquake occurs ... Show more content on Helpwriting.net ...
The main reason for humans are collapse of buildings,landslides, and tsunamis. Animals can sense shakes. They can feel the seismic waves before us.
There are various reports which shows that they start acting strangely, very restless, nervous and frightened. Earthquakes environmental effects are
surface faulting, tectonic uplift, subsidence, soil liquefactions, ground resonance, landslides, and ground failure. Primary effects of shakes are property
damage,loss of lives,fire,and tsunami waves. Some secondary effects are economic loss, disease, lack of food, and clean water. "The effects on the
ground in the intensity scales, by Terra

Compare And Contrast Earthquake And Miami Earthquake
Earthquakes occur daily as plates of lithosphere travel on asthenosphere; however, some earthquakes are larger and cause more damage than others.
Major earthquake zones include the circum–pacific region, Indonesia to Europe, Caribbean and Sandwich Islands, mid–ocean ridges, and East Africa.
Larger earthquakes are rarer than smaller earthquakes, yet when they do occur, they are memorable. The Japan earthquake of 2011 and the Haiti
earthquake of 2010 are memorable for unfavorable circumstances, yet are excellent sources of study for seismologists and geologists. March 11,
2011–– Japan experiences one of the most devastating earthquakes recorded. The epicenter, located at 38.297 N, 142.372 E, produces a magnitude 9.0
earthquake at a depth ... Show more content on Helpwriting.net ...
In addition to the aforementioned information, the tsunami is also devastating to the Japanese population, as well as nations surrounding the Pacific
ocean. In fact, the tsunami is the greatest cause of damage during the quake. In the tragic event, 15,890 people perished, 2,590 people reported missing,
and 6,152 people suffered injuries in Japan–– most of which as a result of the tsunami. The 2011 Japan earthquake could not have been prevented, since
natural disasters cannot be avoided, nor predicted; however, several steps could have been taken to reduce the number of buildings damaged. The
Japanese government possesses good communication with their people (hence the issued tsunami warning), so the loss of life could not have been
avoided. Despite strong communication with the public, the Japanese government could implement building regulations to withstand severe
earthquakes and issue an "early warning" messaging system because sometimes, seconds make a difference. Today, the Japanese government is actively
working to reduce the amount of nuclear power plants to avoid future complications with radioactivity and public health. January 12, 2010, 4:43 p.m.
local time –– 25 kilometers southwest of Port–au–Prince, the capital of Haiti, the earth ruptures (18.44 N, 72.57 W) 13 kilometers below the surface.
Occurring on the Caribbean plate, particularly the

Essay On Earthquakes
Earthquakes: A Natural Hazard
Introduction to Earthquakes
An earthquake is a natural hazard that causes death and destruction. Earthquakes mainly occur on the boundary of two tectonic plates, known as fault
lines, as the plates move against each other and get stuck which creates a strain and results in rocks breaking. This releases energy into the lithosphere
(crust and upper mantle) causing shaking of the earth's surface. The energy released is called seismic waves and these are measured on a logarithmic
scale called the Richter scale.
В¬В¬В¬В¬В¬
Effects of Earthquakes (human or physical)
Ground shaking and unstable buildings are some of the short–term physical effects that are caused by seismic waves. Fires can be created when a ...
Show more content on Helpwriting.net ...
As well as that they should try to find a place that is safe; supplies such as bottled water and canned food should be easy to reach. Communication
systems can be affected so most will set up plans for contacting friends and family.
Immediately after an earthquake looting often happens as many will be without supplies however some people react very differently and try to help
as many people as they can. Countries around the world will send money and food; some may even send volunteers to help and administer first aid.
The rubble will be cleared to free the people trapped. Buildings being made safe is another way they would help but depending on the country's
funding it doesn't always happen immediately. Tourism may decrease as the tourists could be scared of another earthquake or aftershock occurring.
Long–term responses would be things like building restoration because aftershocks are not unusual. Before or after restoration begins an investigation
may be required to figure out why the building collapsed and if there were any faults in construction. The economy will be negatively affected as
rebuilding is costly and normal work is prevented from happening for quite a while. Whilst there are investments made for rebuilding and aid is sent in
the immediate aftermath, families may struggle with reduced incomes and replacement of clothing and household items.
Case Studien
Japan
The TЕЌhoku earthquake is a prime example of an earthquake creating a tsunami. With a magnitude

Earthquake And Earthquakes Essay
4. EXPLAIN THE RISK AND NATURAL HAZARDS EARTHQUAKES AND VOLCANIC ACTIVITIES. HOW CAN WE PLAN TO CONTROL
THESE RISKS?
Earthquakes and volcanoes have disastrous effects on humans and properties, it's also very harmful for the environment overall including wildlife.
Earthquakes cause a lot of damage due their shaking nature,they can further lead to tsunamis and most common hazard related to earthquakes is
landsliding. The earthquake intensity is what measures the effects it has on land surface, and this depends on the rock types and actual ground
displacements, it's measured by the Mercalli scale and bases on human reports of damage experienced. It's interesting that earthquakes of the same
magnitude can cause different amounts of damage ... Show more content on Helpwriting.net ...
Plate tectonic activity is related to many other things like, volcanoes and earthquakes. These natural hazards can be found in linear belts around the
globe. There are seven large plates and many small ones, the main types of plates include the divergent plate boundary (pulls away), convergent plate
boundary (move towards each other) and transform plate boundary (slide past). Ocean–continent boundaries create earthquakes up 700 km deep and
forms seafloor trenches, it leads to andesitic volcanoes in mountain ranges. Yellowstone is a 'hot spot' this is where heating and igneous activity occurs
within crust. Although, not all plates move at the same rate, they are relative to each other. Continent– continent boundaries with divergent can form
rift valleys, earthquakes less than 100 km deep, and basaltic/rhyolitic volcanoes. At Convergent they have young mountain range, 300 km deep
earthquakes, and no volcanoes. At transform, they have a fault zone, less than 100 km deep earthquakes and again no volcanoes. With ocean–ocean
boundaries there is oceanic ridges with rift valley, less than 100 km earthquakes, and basaltic pillow lavas at divergent. On convergent there are
seafloor trenches, 700 km earthquakes and andesitic volcanoes in island arc. With transform you have ridges and valleys in oceanic crust, less than 100
km earthquakes, and some basalt. Plates are driven by the convection in the mantle and movement of the lithosphere.
6. WHAT ARE HURRICANES? EXPLAIN THE

Dangers Of Earthquakes
1. What are some of the dangers of having an earthquake in large cities? There are many significant dangers of having earthquakes in large cities such as
– Large amounts of people being at risk
– Lots of large structures such as buildings
– Set off landslides
– Tsunamis
The devastation of the Earthquake can differ depending on the location and environment of the country the Earthquake occurs. Countries that have
fault lines close to the ocean are more at risk of having large Tsunamis. These waves can reach speeds of up to 500 kilometres per hour and cause
massive devastation to anything in their path (ABC 2017). Some places such as New Zealand are more likely to have things such as landslides since
the country has large amounts of hills and countryside.
2. What are 2 ways to make building that survive earthquakes? You may include a diagram to help you explain. 1. Buildings are designed to support
the walls, roof and all the stuff inside to keep them standing. Earthquakes present a lateral/sideways, load to the building structure that is a bit more
complicated to prepare for. One way to make a simple structure more resistant to a quake is to tie the walls, floor, roof, and foundations into a rigid box
that holds together when shaken by a quake (Imagination Station 2017)
2. Using materials that can bend without breaking helps make buildings more shock absorbent. Materials such as steel being embedded into the walls
can make a

The Disaster Of A Earthquake
The year 2010 was an active year for earthquakes and other natural disasters, racking up a total of four earthquakes ranked 7.0 or higher. Two of
these quakes were merely a month apart, and started the year in a very destructive way. The first was a 7.0 in Haiti, the second over 3,000 miles away
in Chile, an 8.8. Though both ravaged their countries, one was decidedly more devastating than the other. Looking at the magnitudes of the quakes, you
might think Chile received the worst of it, but after further inspection, you may not be so sure. While the magnitude of a quake can be a big factor in
the corresponding effects, the infrastructure of the affected area plays an even larger role in the number of casualties and the amount of devastation
that is experienced. This devastation is further increased in coastal areas due to the high likelihood of tsunamis shadowing high magnitude quakes.
The evening of January 12, 2010 was met with tragedy as a powerful 7.0 earthquake rattled the coast of Haiti. The epicenter of the quake sat close to
the town of LГ©ogГўne, a mere 15 miles from the island nation's capital. (brittanica.com) Many buildings collapsed or were severely damaged,
including the national palace and the United Nations headquarters. The loss of life was unfathomable and death tolls only seemed to grow as the
injured struggled to find medical aid and volunteer relief systems from other countries grappled with the country's lack of proper infrastructure. Haiti's
electrical

Earthquakes Disasters Caused By Earthquakes
Earthquakes are an unfortunate consequence of, well, living on earth. While other hazards such as volcanos, tornados, floods, and wild fires all have
clear visual indications that allow for us humans to get away from them, earthquakes are much more insidious than the aforementioned disasters
because they have no such indicator and the damage they inflict is near instantaneous. Luckily for us humans, seismologists have spent a good portion
of the 20th century finding out why earthquakes occur, how to predict earthquakes that have not happened yet, and how to minimize damages caused
by earthquakes with the help of extremely talented structural and seismic engineers. Our group will be examining four specific earthquakes occurring
near Plate Boundaries that have had a significant impact on nearby communities, the damages and loss of life caused by these earthquakes, and how the
communities that live near hotspots have adapted to the omnipresence of seismic activity.
The first earthquake we will be talking about is the largest earthquake to occur within a U.S territory and the second largest recorded earthquake on
earth, the Alaskan Good Friday Earthquake. The earthquake, lasting approximately 5 minutes, occurred Friday, March 27th at 1736 local time and was
caused by the subduction of the Pacific Plate under the North American Plate. The epicenter of the Good Friday Earthquake was near the Prince
William Sound in the South Central region of Alaska, 76 miles east of Anchorage and

Earthquakes : Volcanoes And Earthquakes
Volcanoes and Earthquakes are Sisters, Not Twins
Volcanoes and Earthquakes are two of the most intriguing natural disasters that can occur on earth. Unlike hurricanes and tornadoes, they can awaken
at almost any point in time throughout the year. These two natural disasters are also different from others because they occur on the layers of the earth
itself. Volcanoes, while large to us, are actually small, conical patches of earth that spurt and ooze hot molten lava from the core, and can destroy
areas of land triple their size. Earthquakes, on the other hand, are severe jolts felt on land due to the movement of earths tectonic plates. Some may
describe earthquakes as being similar to riding a bike down a flight of stairs. The impact of an earthquakes can take down even the largest buildings
and strongest structures. All natural disasters can have damaging effects on land, some more than others, and all can be measured or predicted in
different ways. Although earthquakes and volcanoes are similar to each other, the two are still very comparable. A few of these similarities and
differences include the cause of their occurrence, and how their occurrence impacts the environment.
Earthquakes and volcanoes are both similar in the fact the earthquakes can cause volcanoes to form or even erupt, but the severity of their damage is
caused by different factors and result in different outcomes. The earth can be structurally compared to an egg. It has a large hot core, a thick layer of

Earthquakes In California
Dangerous tsunami threatens off U.S cost
Researchers have found that if a 9.0 magnitude earthquake strikes the U.S's california there is a great chance that a tsunami will occur. If that
happens it will cost over 70 billion dollars to repair. People around that area would only have a 15 minute notice to flee. It could destroy roads,
power lines, bridges, towns, and so much more. Over 100,00 people would die at an estimate. There has been two major earthquakes. One of the
earthquakes was on a sunday and at a 6.8 magnitude and the other one in 2005 was at a 7.0 magnitude. In california there has been six earthquakes
over a 7.0 magnitude or greater in the past 100 years. Scientists have focused on the 9.0 earthquake and the tsunami in japan in

Earthquakes In Texas
Earthquakes in North Texas have been popular in the past couple of years. Texas has never been a state to host earthquakes like the ones being
experienced. There has been many theories from locals about the causes of minor earthquakes. What are their theories about the increasing in
earthquakes in North Texas? One, is the Hydraulic "fracking", the drilling that effects the underground soil to crack. It only gives airways for gas or
oil to work its way up to the surface. The theory of hydraulic fracturing does not add up for some but that the wastewater disposals theory is a better
conclusion. Wastewater disposals or water injections are related to "fracking" institutions. Wastewater disposals are water tunnels filled from
underground that can

Earthquake Intensities
Earthquake Intensities
Earthquakes are a marvel of geology. When faults under the surface of the earth move, the ground moves. These earthquakes can be very mild, barely
registering or they can be horrific with far–reaching consequences. Scientists have become fascinated with the study of earthquakes for centuries but it
is only in recent years that quantified data has been collected and analyzed by scientists regarding these geologic phenomena. Before the invention of
the Richter scale, less accurate means of measuring an earthquake's intensity were used by geological scientists.
Until the early 1900s, earthquakes could only be measured after the earthquake had ended and then only approximations could be made. The first
attempt at scientifically measuring an earthquake's intensity was performed in the middle of the nineteenth century. In Italy in 1857, the after effects
of an earthquake were quantified (Lutgen 2011, page 179). A map was created to show the comparable damages that were found in different areas. This
allowed geographers to make maps which would show the areas of highest intensity and how intensity lessened in surrounding areas. Although this was
helpful, it only showed comparative intensities, not quantified data.
In 1902, Giuseppe Mercalli developed what was called the Modified Mercalli Intensity Scale. An American version of the Mercalli system was
incorporated in 1931. This system judged intensity of earthquakes based upon the ways California

The Causes Of The Earthquake
In the blink of an eye, everything can change. From a monstrous magnitude–9 earthquake, to a series of terrorist attacks, to migrating from a
third–world country that is dangerous to live in, any experience can transform a lifestyle forever. The earthquake that took place occurred in
Fukushima, Japan in March of 2011 took the lives of 15,894 people, as well as leaving 6,156 injured and 2,546 missing. This monstrous disaster
unleashed a raging tsunami that wiped out the east coast of Japan. The tsunami initiated a nuclear disaster that released highly toxic wastes into the
atmosphere, making it dangerous for civilians to be outdoors. The terrorist attacks of September 11, 2001 were a series of four coordinated attacks by
the Islamic terrorist group al–Qaeda that place in New York City and Washington D.C. taking the lives of 2,996 people. The U.S.
– Mexico border has
approximately more than 7,000 deaths from people attempting to cross the border since 2000.
In the midst of the terror, one can learn lessons to last them a lifetime. The people who lived through these events went through a series of obstacles,
both mentally and physically. For all three of these occurrences, there were a vast amount of family members lost, which is never an easy pill to
swallow. Nothing defeats the mental hardship of leaving one's grandmother behind in order to escape and survive a tsunami. In the midst of these
disasters, there were instances of both selfishness and selflessness. From loss of

Earthquakes Essay
Earthquakes
Throughout history, man has made many advancements. These advancements have been made to make life easier. The one thing man can't do is to
control Mother Nature. Mother Nature can cause many things such as earthquakes.
The causes of earthquakes have been theorized in many ways. According to the book
Predicting Earthquakes by Gregory Vogt, the Greeks, "blamed the earthquakes on Poseidon, god of the sea"(25). The Hindu believed that "the earth
was a platform that rested on the back of eight great elephants. When one of the elephants grew weary, it lowered and shook its head causing the
ground above to tremble"(Vogt 25). Margaret Poynter writes "many primitive people thought that the earth rested upon the back of some... Show more
content on Helpwriting.net ...
He made tests, drew a world map, and recreated earthquakes only to find that rocks are being overstressed at the faults. "A fault is the place where
two plates meet and are rubbed against each other" (Groiler Electronic Publishing,
Inc.). The book, Predicting Earthquakes, the author points out "There are generally three kinds of faults: normal, reverse, and strike–slip. By careful
observation and measurement, geologists, acting like detectives, can tell how much a fault moved, which part went up, which part went down, and
which way the fault moved" (Vogt 26). "When one of the plates slip under the great amount of stress at the fault, anearthquake occurs. The shaking we
feel are the passing of long waves" (Putnam 443). "The L–waves (long waves) travel at slower velocities that the primary and secondary waves. These
waves make the largest squiggles on a seismograph but their effect diminishes rapidly with distance. The L–waves are limited to the crust" (Putnam
443).
One of the two kinds of waves are "Primary waves are a kin to sound waves, and thus produce alternate compression and rarefaction in the medium
through which they travel much like the waves that spread out through the air in all directions from a tuning fork" (Putnam 444).
The second of the two kinds of waves are "Secondary waves, the particles in the rock through which the wave is traveling vibrate at right angles, or
transversely, to the direction of

Essay On Earthquake
The data from nine earthquakes happened in winter and summer time, with magnitudes ranging from M 3.0 to M5.7, was collected at a sampling rate
200 Hz and preprocessed for the further analysis [4]. Then, dynamic properties of the structure were obtained using modal property identification
toolbox (MPIT 2.0) developed at the University of Auckland [13]. The modes were determined from the following system identification algorithms:
–Frequency domain methods: the peak picking (PP), the frequency domain decomposition (FDD), the enhanced frequency domain decomposition
(EFDD) –Time domain method: stochastic subspace identification (SSI) method [14] identifying the stable poles by generating singular values around
them from the singular value... Show more content on Helpwriting.net ...
Then, the most plausible modes was chosen by comparison of MAC values of each date for each SI algorithm. Since fundamental mode of the
bridges always excited by the translational ground motions during earthquakes, transverse components of mode shapes only were described in this
research to estimate the input of different bridge components on the bridge dynamic response. The frequency values obtained by each method,
except of SSI for summer dataset, at each season and their mean and coefficient of correlation are shown in Table 3.1 and Table 3.2. From this
figure, the values of fundamental transverse frequency identified by each method are highly correlated for all methods, the mean coefficient of
variation was no more than 0.02. In addition, no relationship between the transverse frequency and the depth of frozen soil at specific dates was
observed. A high correlation between mode shapes, with MAC value 0.95 or higher, was observed for two frequency domain methods only, FDD and
EFDD. Therefore, the average values of natural transverse frequency calculated from the values identified by each method, 7.69 Hz and 2.85 Hz, and
mode shapes obtained by FDD technique (Figure 3.1) were chosen as a baseline experimental values for the further calibration of the numerical models
developed for winter and summer respectively. The bridge transverse response is mainly symmetrical; the possible

Miami Earthquake
Vietnamese people have a sentence that is "Fire tests gold, difficulties test strength". Indeed, Japan is one of the best developed countries in the
world, even though Japan meets horror earthquakes and tsunamis average every year. In the picture above, we can see that a half side of village in
Japan was under water and some houses seem like disappear in the water influx, while another side is still above, and water still continues pouring to
submerged the village. Outside of the village, there are lines of trees which seemed like want to protect the village, but it was impossible to do it.
Because of the water pressure, the rest houses started breaking; the electric columns also fall down alternately. Luckily, all of people was announced that
... Show more content on Helpwriting.net ...
The first many waves of tsunami hit Japan's coastline which was 60 kilometer in offshore East Tohoku coast. The massive tsunami suddenly appeared
and submerged everything along the Pacific coast of archipelago northern Japan. "The tsunami waves reached run–up heights (how far the wave surges
inland above sea level) of up to 128 feet (39 meters) at Miyako city and traveled inland as far as 6 miles (10 km) in Sendai. The tsunami flooded an
estimated area of approximately 217 square miles (561 square kilometers) in Japan" ( ). Also, near Oarai, the tsunami generated a huge whirlpool
offshore. The Tohoku to destroyed and immersed a lot of houses as well as high buildings. In addition, the Tohoku tsunami not only happened in Japan
bit also spread across the Pacific at least 20 countries, including the western coast of North and South America. However, though it can affect many
parts of the region, but it caused only relatively small impacts; Japan was the only countries that had to be influenced heavily. Although Japan had
warning actions and rapid evacuation, they cannot avoid and reduce

The California Earthquake
In the article "What will happen when the "big one" hits California?" it's focused
on the effects and what might happen to make the audience be more interested and want
to keep reading the article. By making the title a question it makes the article more
persuasive for the audience to get the answer. It uses ethos to appoint the statements
stated. The article was very well put together and had a good format which made it easy
to read. Includes links and other sources to back up statements also includes an
illustration.
"The big one" is referred to as the earthquake that could happen. On March 17,
2014 there was an earthquake with a 4.4 magnitude in California. It shook the ground
which made even the news anchors to duck ... Show more content on Helpwriting.net ...
The article is written on a trendy website. The author uses a serious tone
throughout the whole article and has different sources in it also like the LA times
article link included. He does although add in a little humor and says "If you want a
good laugh check out the video I posted below" which is a video of the news reporters

live when the earthquake occurred and how the studio shook and they bent down
under the table. They get up and notice that actually even some of the stuff from the
ceiling fell down and the screen behind them was still shaking. After the earthquake
passed they went to their other live reporter that was in Los Angels and he told them that
about 10 seconds after the earthquake hit LA.
In conclusion, The article wanted to point out that California could be in serious
damage and the effects could be drastic. It wanted to grab attention to the people that
live in California. He caught the attention of readers by the title. The text was
straight–forward and other sources were included. Over all the article was very
informative and it was created to address the issue or the possibility that might

Earthquakes With Earthquakes
Earthquakes: The Same Effects, but Different Responses
Earthquakes occur as a result of the abrupt release of energy in the Earth's crust that creates a series of waves known as seismic waves. Earth quakes
greatly affect people whether they are living in economically disadvantaged countries or in economically developed countries. However, the way each
of them responds to the hazard is different.
The tectonic movements in the earth's crust are the initial causes of earthquakes. These movements bring about forces of tension and pressure, these
forces stress up the earth's crust. As the stresses increase, an imbalance in equilibrium of the rocks which results into breaking of rocks and
displaced. The energy accumulated during the process is released giving raise to waves. The waves cause vibration of objects they come across with
causing a lot of impact on them. This may include shaking and rapture of the ground. As a result there is damage of infrastructure, landslides, fires due
to damage caused to electric and gas lines.
Volcanic eruptions can also cause earthquakes since they are often very violent and can cause vibrations to the earth's crust, this can result into rupture
of geological faults. This is as a result of the movement of lava beneath ... Show more content on Helpwriting.net ...
This is due to the fact that LEDC are economically disadvantaged as compared to the MEDC which tend to have a quicker response and recovery from
earthquake damage. Take a look at the Los Angeles earthquake of 1994 and compare it with the Kashmir earthquake of 2005, one will realise that
the responses were totally different. In Los Angeles almost all schools had been opened in a period of just one week, and in three weeks all schools
had been opened. However, in Kashmir it was distinctively a different case, whereby rebuilding and re–supply of schools took much longer than three

The Earthquake
The Earthquake
It was a sunny day outside. The heat from the sun was hitting my face as I was painting the hot summer day onto my canvas. The colors made the
image stand out and made it bright. The yellows added the joy to the picture while the greens freshened up the image. It was burning outside and
my throat felt dry, like the Sahara desert. I reached for my cold cup filled with icy lemonade. I slowly took the last sip. I felt hydrated as the ice
cubes were hitting my lips and little bits traveling down my throat. My palms were covered in water drops from the cup. I went back to painting after
I dried my hands and gently wiped my lips with a soft napkin. After painting for awhile I decided to take a small break. I held my cup tightly and ran
downstairs with little drops dripping from the cup. There was just a little bit of lemonade left so I decided to carefully pour the rest into my cup and
head upstairs to my room. As you may know almost everyone has siblings, including me. While my parents were not home, I was painting my
beautiful picture, my older sister decided to show up. Her name is Jasmine. She's fifteen, with long, brown locks, spring green eyes, and pale skin
with freckles sprinkled on her nose and her rosy cheeks. She was beautiful but her soul wasn't. I could feel something was up as she bursted through
my door. "I can't believe you drank the rest of the lemonade you selfish pig. Ugh I hate you so much. I hope you die." she shouted as she

A Brief Note On The Earthquake Of Earthquake
Abstract
Earthquake engineering is a subject where a person can be overwhelmed with information but still crave for knowledge due to its unpredictable
nature. Earthquakes are a natural repetitive occurrence on planet earth, which due to its devastating impact, have caused a lot of damage to
structures and caused loss of life. Therefore engineers, scientists and geologists were required to take action and one of the many first steps was to
identify the regions of seismic activity. The argument in this essay is not how to prevent earthquakes as that is out of the control of humans but how
to minimise the damage and deaths caused by them by designing better buildings. The challenge to first achieve this goal was by engineers in
America, where in 1906, in the state of California, due to the frequent earthquakes in the state, building design codes and safety standards were
established. These design or seismic codes have helped to reduce the damages caused by earthquakes. Therefore the solution for people in active
seismic zones is to adhere to the seismic codes strictly, designed by engineers in order to help strengthen buildings and reduce the loss of life when an
earthquake occurs.
The greatest number of earthquakes occurs in Asia, America, Caribbean Islands and Europe but according to Hyndman, D and Hyndman, D (2012),
earthquakes do not actually cause the death of people but the falling debris and buildings do. This is why it is important for engineers to use

The Earthquake Of Christchurch Earthquake
An analysis on the mechanism of destruction, impact, recovery, responses and future steps of the 2011 M6.3 Earthquake in Christchurch, New Zealand.
Helena (Jiahui) Zhang
250641678
November 18 2014
Geography 2152F
Mark Moscicki
Table of Contents
1.0 Description of Event 2
2.0 Causes3
3.0 Impacts5
4.0 Responses7
5.0 Recovery8
6.0 Suggestions for future steps 10
7.0 Bibliography 11
1.0 Description of the Event
The Christchurch earthquake with a magnitude of 6.3 (Ritcher scale) hit New Zealand's second largest city, Christchurch, on February 22, 2011 (Fig1).
Figure 1. Map of New Zealand.
In red the affected zone of Christchurch earthquake (Earthweek, 2014).
It's recognized as the second deadliest earthquake in New Zealand following the 7.8 Hawkes bay Earthquake (Kaiser et al, 2012). The earthquake
was first thought to be an aftershock of the 7.1 Darfield earthquake of September 2010 at the eastern edge. This was an area that originally was of a
low earthquake occurrence rate since prior to 2011 there was no knowledge of a fault's existence thus catching the New Zealand citizens off–guard. The
Christchurch earthquake resulted in 185 casualties affecting more than 300,000 people (Kaiser et al, 2012). The earthquake first made contact with in

the South Islands, only 10 km away from the center of Christchurch. Ground motions were unusually large near Christchurch measuring 2.2 g and 1.7g
at the epicenter, the point directly above

Earthquakes In The Odyssey
The thought of massive tornados, earthquakes, tsunamis, and other natural being the result of a powerful Greek God is simply perceived as a
story in our modern day world, but this was no natural phenomom to the people of ancient Greece. In Homer's great poem The Odyssey many of
these natural phenomenons were created by the powerful Greek Gods, while in the modern day article Are earthquakes on a rise? Is California's
'Big One' coming? written by Holly Yan a focus of scientific evidence and years of expert research have revealed a much more probable and realistic
cause of these disastrous events. In the Odyssey, Odysseus faces many of these natural phenomenons on his journey home to Ithaca, all of which were
purposefully created by the Greek... Show more content on Helpwriting.net ...
Some of most notable events that manifest these major differences of thinking between these two periods of time consist of the acts of poseidon
being the cause of treacherous weather conditions at sea resulting in the setback of his return home, Zeus washing Odysseus boat up to shore and the
bag of wind given to Odysseus by the God Aeolia as a one way ticket back home.
Poseidon created a major setback of harsh weather conditions for Odysseus and his crew out of anger and vengeance for his son Polyphemus after
Odysseus shot an arrow in his eye leaving him blind. As the God of Sea, it is believed that Poseidon has the power to create unimaginable storms
and in this case a storm so strong its outcome delayed Odysseus voyage home by years, but modern day science proves otherwise. " Hear me,
Poseidon who circle the earth, dark haired ... let him come late, in a bad case, with the loss of all his companions, in someone else's ship, and find
troubles in his household " (Homer 9) Polyphemus knew that his anger towards Odysseus actions could quickly be resolved by the assistance of his
father's powers. This shows to prove that the ancient grecian people's religious culture is greatly based on the doings of the Gods, and has greatly
impacted their way of thinking. The possibilities of other causes was very

Belconnen Earthquake
On Saturday, the 3rd of November a 6.0 earthquake hit the Westfield Belconnen mall in Canberra. The earthquake frightened many in the mall and
went outside. The damage that was caused inside the epicenter was moderate. Pictures and books in stores fell down. Dishes, glass wear and windows
were broken during the earthquake. Some of the heavy furniture was moved around during the earthquake. Plaster in the mall varying between
considerable and large amounts. Chimneys cracked and some of the walls cracked. Some tiles and bricks were loosened and the corner to the 1st
entrance way came off. Major destruction was caused to the weakest parts of the mall. Water pipes in the mall were ruined and the electricity stopped
for about an hour, which was disruptive for shops that had electrical appliances or stores that sold game consoles and computers. Stores that had food
in them had to shut down and remove the food. They then had to find other places to store the food since fridges weren't working. There was also
some damage that was outside of the epicenter. The damage spanned ... Show more content on Helpwriting.net ...
Homes may be destroyed. Transport and communication links may be disrupted. Water pipes may burst and water supplies may be contaminated.
Shops and business may be destroyed. Looting may take place. The damage to transport and communication links can make trade difficult. The built
landscape may be destroyed. Fires can spread due to gas pipe explosions. Fires can damage areas of woodland. Landslides may occur. Tsunamis may
cause flooding in coastal areas.
Long–term impacts Disease may spread. People may have to be re–housed, sometimes in refugee camps. The cost of rebuilding a settlement is high.
Investment in the area may be focused only on repairing the damage caused by the earthquake. Income could be lost. Important natural and human
landmarks may be

Compare And Contrast Earthquake And Chile Earthquake
The Chile and the Haiti Earthquakes of 2010 had different effects on the health sector. Various differences are evident in the health outcomes of these
disasters. In the Chilean earthquake, the magnitude of the quake reached a scale of 8.8 while that of Haiti reached a scale of 7.0. However, the
number of deaths that were experienced in Haiti was a number almost 200,000 while in Chile it was only 200 people (Huus, 2010). Despite the high
magnitude of the quake, Chile experienced a low number of lost lives. The major reason for the difference in the number of casualties are the
differences in the building codes. The building codes provide rules that specify the standards of construction of buildings. In Haiti, there are no building
codes, hence ... Show more content on Helpwriting.net ...
Most of the people succumbed to diseases that arose from the sanitation, infections, and other health related issues that occurred after the disaster. This
is because they lacked their own mechanisms of combating infections, sanitation issues, and post disaster mental issues (Huus, 2010). They also lacked
response plans for a disaster of a higher magnitude. For example, there was no disaster management system that showed the various protocols of
managing a large–scale disaster. Therefore, health issues such as sanitation, comfort, and management of communicable diseases was a major problem
(Farmer et al 2011). Other factors responsible for this problem is the high level of poverty, lack of infrastructure, and the large population. In Chile,
there were established mechanisms of managing the disaster. There were health interventions that were available, including rescue teams, preventive
techniques, sanitation and other disease management protocol. For example, organisations such as AmeriCares delivered about $730,000 in medical
aid that included 2,000 hygiene kits. This enabled the effective management of the health concerns, hence management of comorbidity from the
disaster itself (Candia,

Kobe Earthquake
Murakami Haruki had a method with his stories, that captivated his audiences through the complexities of his plots as well as the obscure meanings
within them. One of his stories, in the set of after the quake takes place in February 1995, after the disastrous Kobe earthquake. In this story,
"Super–frog saves Tokyo", Murakami chronicles the reactions of a disaster such as the Kobe earthquake through the narrative of a frog trying to save
Japan from a worm that will cause an even more disastrous earthquake. Through this narrative, the portrayal of the animal protagonist, can be
interpreted as a portend for both disaster as well as transformation. Through the use of Katagiri's encounter with the frog, Murakami shows the
instability of life and ... Show more content on Helpwriting.net ...
Frog appears and explains that the fight took place in his imagination which brings up magical realism again and questions reality. The fact that
Frog is exhausted and wounded shows the reality of the event through the circumstance of the frog explaining that Katagiri did help by leading the
way with a foot powered generator. Frog explains that he is unable to defeat the worm but held it off in a draw enough to prevent the earthquake.
This reality is quickly questions by the fact that frog tells him that the battle took place in the area of imagination. This magical realism is
exemplified at the end when Frog slips into a coma and the disturbing image of boils popping and maggots and worms crawling out of the body. The
insects fill the hospital room and Katagiri screams, but when the nurse turns on the light, the insects and frog are suddenly gone. Katagiri is delirious
but he believes that frog sacrificed himself to save Tokyo from the earthquake. Alex Bates might use this sacrifice as evidence for his claim, but I
would argue that, again, the frog's representation at the end while he is disintegrated into insects, shows the rejuvenation and transformation of
Katagiri. Katagiri is able to rest easy after this happens as he is satisfied to have participated in such a glorious battle after having spent his life being
boring. Frog

The Next Earthquake
Imagine the lives and money we could save if you could predict when the next earthquake will hit. To bad that world is at least a century away. The
technology and are study on the earth and tectonic plates isn't all there yet but at the rate we are advancing as a species we will quickly get the
technology to easily predict quakes. "We already have the tectonics plates mapped out", says Joel Achenbach in her article "The Next Big One".
With having the tectonics plates already mapped out we know exactly where they already are. All we need to know is how fast each tectonic plate is
moving and what direction they are going to see when the next quake will be. Scientist will be able to calculate when the next earthquake will hit
because by having

The Earthquake Of Nepal Earthquake
Earthquakes are destructive natural disasters that have the potential to occur. Earthquakes greatly impact various locations around the world. Generally,
earthquakes typically only last for a few brief moments but they can greatly impact a society. One of which include the Nepal Earthquake of April
25,2015. This particular earthquake flattened large parts of the capital Kathmandu and also, caused destruction throughout the already improvised
Himalayan nation. The earthquake in Nepal was the most catastrophic natural disaster in the last 80 years (News Discovery, 2015). With this in mind,
the Nepal earthquake obviously has caused a tremendous amount of damage and loss. However, earthquakes are bound to take place due to Mother
Nature. In order to understand the severity of the earthquake in Nepal, it is imperative to comprehend how earthquakes form. While much of the
damage in Nepal could be attributed to the country's poor infrastructure, citizens in other nations can mitigate the disastrous effects of an earthquake by
becoming knowledgeable of natural disasters. Thus, this paper will explain several different aspects regarding how earthquakes form, the severity of
the Nepal earthquake, and how earthquakes can be mitigated. Ultimately, to fully comprehend a specific earthquake one must know how earthquakes
form as well as, how they work. An earthquake is the shaking and vibration of the Earth 's crust. This happens when two blocks of the earth suddenly
slip past one another

Earthquakes In America
Because of the mass number of Hurricanes that have hit Texas, Puerto Rico, and Florida a majority of AMericans are focused on cleaning up the
damages caused by the hurricanes and hoe to be better prepared when the next one comes. Because of this the American population is too preoccupied
to focus on other matters at hand. If we pay attention to the recent earrthquake that took place in Mexico City we can see that the hurricanes aren't the
only thing we should be worried about. The United States seems to focus mainly on hurricanes, rather than on earthquakes, solely for the reason that,
especially recently, hurricanes have caused havoc among the citizens of America. Because of the fear that America holds towards hurricanes they are
so focused

Earthquake Dbq
Imagine if you had to restart your life, new shelter, new job, new lifestyle. Well locals or people in the Philippines had to restart their life when an
earthquake with an magnitude of 7.1 hit the country and destroyed people's lives. The earthquake had a devastating 7.1 magnitude. The earthquake hit
the Philippines on October 15th, 2013. The likely culprit of the earthquake was the East Bohol Fault because the two tectonic plates were sliding
against each other and the creates an earthquake. Sadly, earthquake killed more than 90 people. Ports, schools, and airports were damaged. A hospital
collapsed then that lead to a killing of 18 people. Children were also injured at sports complexes because people rushed the exits when the the ground
started to shake. Lastly, 5 people were killed in a landslide that was triggered from the earthquake. What really matters though is how people respond to
the ... Show more content on Helpwriting.net ...
One example, Children of Sto. Nino Foundation, the Tupas Chapter foundation, and other people from other countries donated money to give
financial assistance to people in need.(Doc B) On December 26, 2013, the IFRC issued a revised emergency appeal seeking 8.5 million US dollars
to enable the Philippine Red Cross to assist 20,000 families for 16 months. The response to the appeal has been slow, but they have still collected 2.3
million us dollars to assist 1,200 families.(Doc A) An organization from Cebu, named Bangon, donated tons and tons of pounds of food to people in
the Philippines.(Doc B) The reason the organization knew to donate food because they heard about the earthquake, and people in the Philippines
seeked help from other countries. It's crazy how these people who are going through such a hard time are getting out and gathering so many supplies.
There getting help from others and and then they're putting those goods to good for

Earthquake Dbq
An earthquake is where two transform plate boundaries slide and creak the earth. This is what happened in the Philippines. Although it was in 2013
the people are still in need of help to get back to their daily lives. The Philippines earthquake had a magnitude of 7.1. This earthquake was gigantic,
and it took down many buildings that were in its path. Lucky the children were not in school that day because of the Muslim holidays the earthquake
caused the school to collaspe. If the children were in school, then it would have killed most of the kids.There were 2,100 aftershocks. The day of
the quake was October 15, 2013. People respond to a natural disaster by gathering materials and donations, spreading the word, and the
government's aid. People respond to a natural disaster by gathering materials. The Red Cross had provided many of the most needed items such as
blankets, mosquito nets, and water containers (Doc A). People were in great need of these organizations at this time in their lives because people in
families had died, and they were not ready to take on the change of overcoming this tragic time. Some of the most needed items were water and
health care services (Doc A). The people were in need of food, but they had struggled to find it. "Just 10 hours later, food was there" (Doc B).
Although food was there, it was not enough for some people to eat. ... Show more content on Helpwriting.net ...
Some of the first places people saw it was on social media sites like Facebook (Doc B). Some other major places, people saw it was on the news and
in news articles (Doc B). It seemed for people to open up the paper and one of the most well known articles was about the Bohol earthquake. It was not
the thought that counts in this situation, it was the action that did count. In document A, the Gordon said "We are confused with the challenge where
the media and donors seem to have forgotten that there are still massive needs amongst earthquake survivors in

The Valdivia Earthquake: One of the Most Powerful in History

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The Valdivia Earthquake: One of the Most Powerful in History