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Recommended: Earthquakes _____.
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 waves cause vibrations which move perpendicular to the wave.
These waves travel on the surface of the earth and move much slower
than primary waves. Thus, when an earthquake occurs, seismic centers
throughout the world record primary waves before the secondary waves
arrive.
Historical Overview
Earthquakes have captured the imagination of people living in
earthquake prone regions since ancient times. Ancient Greek
philosophers thought quakes were caused by subterranean winds, while
others blamed them on fires in the bowels of the earth. About AD 130,
a Chinese scholar named Chang Heng reasoned that waves must ripple
through the earth from the source of an earthquake.
By 1859, an Irish engineer by the name of Robert Mallet proposed that
earthquakes occurred by either a sudden movement of flexible materials
which formed the earth's crust, or by their giving way and fracturing.
In the 1870s, an English geologist called John Milne invented...
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...nia prepares for the
"big one." Despite the tremendous impact of the Northridge earthquake,
no one believes that it is the last nor even the largest which will
strike the greater Los Angeles area. A new 36,000 square foot
Emergency Operations Center has been constructed in East Los Angeles.
A series of laws and procedures entitled the "Standardized Emergency
Management System" has continued to make the Mutual Aid System even
more effective. The Los Angeles Sheriff's Department has taken a
leading role in establishing courses in crisis action planning, crisis
decision making, command and control, operations, logistics and
intelligence. Liaisons and working groups with other agencies and
disciplines has provided additional insight and contributed to a high
state of readiness as they prepare for the next major earthquake.
Earthquakes are best described as a shaking or vibration of the ground caused by breaking of rock. Sometimes they are very strong and other times you would hardly notice them. This shaking occurs when stress that builds up in the crust is suddenly released as the crust breaks free and/or slides against the other pieces of crust. Earthquakes may also be thought of as the breaking of a popsicle stick by applying pressure to both ends at the same time. Should you try this experiment , you will feel the pressure build up as you apply more force until the stick snaps. When the stick snaps you will feel an instant of pain at your fingers as the stress reduces and energy waves move throughout the stick. When the earth's crust is placed under similar types of stress, binding as the stress builds, it will also snap and release the energy into the surrounding rocks, 'ooch'. Thinking about earthquakes will become more clear if you try another experiment.
Earthquakes are a natural part of the Earth’s evolution. Scientific evidence leads many geologists to believe that all of the land on Earth was at one point in time connected. Because of plate tectonic movements or earthquakes, continental drift occurred separating the one massive piece of land in to the seven major continents today. Further evidence supports this theory, starting with the Mid-Atlantic ridge, a large mass of plate tectonics, which are increasing the size of the Atlantic Ocean while shrinking the Pacific. Some scientists believe that the major plate moveme...
The earth is split into four layers, inner and outer core, the mantle and crust. The top of the mantle and crust make up what is like the skin of our earth (see source 2). The skin is split up like a puzzle and we call these puzzle pieces’ tectonic plates (see source 1). These plates are constantly moving and the plate boundaries (edges of the plates) move and slide past one another. Sometimes as the plates move the plate boundaries become stuck. Pressure builds up in the stuck area over time and eventually breaks. This is why earthquakes occur due to the sudden movement of the plate sliding and breaking creating a fault line to go off. The fault line is the line on which the
Earthquakes have been recorded throughout history for thousands of years. Even before seismographs in early times, there are records and accounts of mysterious ground shaking. Earthquakes occur when rocks break along an underground fault (UPSeis, 2007). This, in return, causes vibrations through the earth which causes ground shaking. The magnitude of the shaking varies depending on how great the movement along the fault is; the greater the movement, the bigger the earthquake. Some earthquakes are huge and cause significant damage, while others are small and cause little or no damage what-so-ever. Earthquakes are unpredictable, and can happen at any time. It is uncertain where an earthquake will strike, but there is a greater risk of an earthquake for areas lying on or near a fault. No one is ever prepared for an earthquake, so the people affected must face a sometimes terrifying reality and can be scarred for life. One country in particular that has been severely affected from an earthquake is Italy. Over a century ago Messina, a city located in Sicily, was to face one of the most devastating natural events of the century.
Boom! Crash! Sound echo everywhere. People scream all around you. A deadly 7.1 magnitude earthquake has just hit your town. On October 14, 2013 this happened in the Philippines (B-Essay). There were 3,512,281 affected individuals and 36,645 houses damaged (Doc. D). 39 roads and 18 bridges were in disrepair (Doc. D). People respond in certain ways after a natural disaster. They band together and react with Red Cross and government, Evacuation centers, and Gathering supplies.
Geology 2400 is a course where students are taught different examination of the earth such as the solar system, interior surface of the earth, atmosphere, and relationships of earth systems such as natural disasters. Three essential concepts I mastered was: earthquake’s wave, the planets, and minerals. First, one scheme of a natural disaster is an earthquake. An earthquake is the violent shaking of the ground which sometimes causes great destructions. Earthquakes happened due to seismic waves. A seismic wave is a wave in the earth that is produced by an earthquake. In addition, body waves play a big role in earthquakes. Primary wave (P), is the fastest and it is compressional meaning it can pass through liquids gasses and solids. A secondary wave(S) is the second fastest wave that is shearing, meaning it can only go through solids. Nest, the surface waves also known as the L waves, travel along the surface. For example, these types of waves look like “ripples” moving vertically up and down in motion. On the contrary, love waves (LQ) are horizontal waves and
Before I begin talking about earthquakes I should explain how earthquakes begin and their results. The movement of the earth plates are the ones that causes earthquakes. It occurs when plates meet along plate boundaries. When they move towards each other, one of the plates can be pushed down the bottom of the other plate, into the mantle. This is consider the subduction zone. When the plates gets stuck, it causes a lot of pressure on the surrounding rocks. The pressure will released and produce shock waves, they are called seismic waves and in other words, this will be called an earthquake. In this essay I will talk about the earthquake in Chile from 1962. I will speak how this earthquake affected the earth and the damages, not only to earth,
Tectonic Activity The continents of the world are all separated by different tectonic plates which when collide is called Tectonic Activity. There are different forms of tectonic activity and different processes and landforms, which are involved during and as a result of the collisions. As and when these collisions are going to take place we can't determine because current technology hasn't allowed us to dig as far into the earth to the point of pressures which causes the plates to collide. These pressures are believed to be eruptions of liquid magma deep inside the earth.
Exploring Why LEDC's Suffer Greater Damage From Earthquakes Than MEDC's A MEDC is a more economically developed country; therefore it can afford to spend money on improving the countries stability and helping to decrease the damage from an earthquake. An example of a MEDC is Kobe, in Tokyo, where in January 1995; an earthquake that measured 7.5 on the Richter scale hit the city. A LEDC is a less economically developed country and therefore cannot afford to spend money to protect the country from earthquakes. An example of an LEDC is Armenia, in Columbia, where on the 25th January 1999; an earthquake measuring 6.3 on the Richter scale was the worst earthquake the country had experienced since 1983.
What are earthquakes? An earthquake is what happens when two pieces of the earth suddenly slip past one another. The surface where they slip is called the fault or fault plane. The location below the earth’s surface where the earthquake starts is called the hypocenter, and the location directly above it on the surface of the earth is called the epicenter, or focus.
Earthquakes play a major role into understanding the composition and materials that exist within the Earth (Merali and Skinner, 2009, p.252). Earthquakes are the main source of insight into the inner workings of the earth, due to the nature of the seismic waves they produce. P and S waves are reflected and refracted at different boundaries within the earth, and this enables seismologists to make inferences about the internal composition and structural of planet Earth. (Merali and Skinner, 2009, p.252).
Hazards pose risk to everyone. Our acceptance of the risks associated with hazards dictates where and how we live. As humans, we accept a certain amount of risk when choosing to live our daily lives. From time to time, a hazard becomes an emergent situation. Tornadoes in the Midwest, hurricanes along the Gulf Coast or earthquakes in California are all hazards that residents in those regions accept and live with. This paper will examine one hazard that caused a disaster requiring a response from emergency management personnel. Specifically, the hazard more closely examined here is an earthquake. With the recent twenty year anniversary covered by many media outlets, the January 17, 1994, Northridge, California earthquake to date is the most expensive earthquake in American history.
Earthquakes are vibrations felt at the surface of the earth which are caused by disturbances of the energy in the earth's interior. These vibrations are known as seismic waves. (Skinner Robinson McVerry 1) There are different type sof seisimc waves such as Primary (P) waves, whcih travel the fastest, Secondary (S) waves which cause the earth to vibrate vertically, Surface (L) waves. P and S waves are "affected by changes in the density and the rigidity of the materials through which they pass." (Columbia Encyclopedia) Earthquakes vary in their intensity and duration. Often times they are strong enough to cause massive destriction. Tall buildings often suffer as a result of these natural disasters. In recent years this has become a larger and larger threat with both the number of large buildings, and their number of occupants increasing. In an effort to try to minimize the damage caused by earthquakes many some engineers focus primarily on designing and constructing earthquake resistant buildings. Earthquake engineers have gathered much of their information from analyzing past earthquakes, and learning which buildings can and can't withstand the tremors. The goals of these engineers is to design buildings that can withstand moderate earthquakes and obtain minimal damage, and that the buildings will not collapse lowering the probability of human deaths.
Earthquakes belong to the class of most disastrous natural hazards. They result in unexpected and tremendous earth movements. These movements results from dissemination of an enormous amount of intense energy in form of seismic waves which are detected by use of seismograms. The impact of earthquakes leaves behind several landmarks including: destruction of property, extensive disruption of services like sewer and water lines, loss of life, and causes instability in both economic and social components of the affected nation (Webcache 2).
It was a beautiful day like any other with the clear blue sky and the