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Impacts of an earthquake
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Recommended: Impacts of an earthquake
Geoffrey Yang
Physics Per. 1
Bennett
w/ Paul Eremenco
How Are Buildings made to be Earthquake-Proof/Resistant?
“Earthquakes alone don't kill people; collapsed buildings do” (Sutter). In addition to possibly causing tsunamis, earthquakes are responsible for releasing enormous amounts of energy that spread through the crust as seismic waves. These seismic waves include P-waves and S-waves. While P-waves do not cause as much destruction due to their vertical movement, S-waves can cause buildings to collapse completely due to the waves’ lateral movement. In addition to collapsing buildings, earthquakes can also cause liquefaction which is when loosely packed soils temporarily behave like liquids, resulting in sliding and sinking buildings (Harris). Earthquakes have been responsible for 60% of all deaths caused by natural disasters in the past decade (Universitat Politècnica de Catalunya).
When designing an earthquake-proof building, certain preparations must be made. Before building design starts, engineers first determine the seismic risks of the location based on historical data. ...
The enormous responsibility that an engineer has when designing a project is often overlooked. His or her job is not only to create a design that will work under ideal conditions, but that will meet the regulations of environmental and building codes and will also survive the unpredictable forces of nature that structures are sometimes subjected to. An article in the Seattle Daily Journal of Commerce, "Structures are Held up by Both Skill and Luck,"1 describes many risks involved in the designing process and the failures that can occur when small details are overlooked. In light of a recent surge of failures in the Northwest, the article says:
An earthquake is the shaking of the ground caused by sudden release of energy inside the earth's crust. It's the breaking and moving of tectonic plates along a fault line. Earthquakes can range in size from weak where we don't feel them to extremely violent where they actually thow people around and destroy cities. They may be a result of geological faults or other activites such as volcanoes, landslides, mine blasts and nuclear tests. An earthquake is not always naturally caused.
Before the San Francisco earthquake, not much was understood about earthquakes like how and where they occurred, or the destruction that could occur and the theory of plate tectonics was over a half-century away. Now scientists can answer the following questions: where a strong quake will likely happen, how probable it is, how intense it will be, how will the infrastructure fare, where to avoid building critical structures, and how do we design and build earthquake resistant structures. Scientists that flourished after this earthquake were Lawson, Reid and Gilbert but the most significant discovery is credited to Henry Fielding Reid, Professor of Geology at John Hopkins University. Most of the building structures that were destroyed or damaged were made out of wood. About 24,500 buildings out of the 28,000 buildings were built with wood structures and the other 3,500 buildings structures were made out of brick. With almost 90 percent of the structures being wood, fires and gas caused most of the
Out of all the natural disasters that we talk about in class, the most deadly would have to be a Tsunami. Compared to earthquakes, Tsunamis have cause more deaths since 1945. A Tsunami is likely to strike anywhere on the west coast, including Santa Cruz in California – United States – North America – 36:58:24N 122:02:09W. A Tsunami is a giant “wave” of water that is caused by a sudden shift in the sea floor. The wave is a result of the water attempting to regain its equilibrium, which is driven by gravity. The size of the wave is determined by how much the sea floor is moved vertically, and how quickly it shifts. A greater water depth helps as well. They can travel up to five hundred miles an hour and have wave heights of one hundred feet. Earthquakes are the leading cause of Tsunamis. People who live in California are well aware of earthquakes that are frequently caused by the San Andreas Fault. However, not many are aware of the results of earthquakes that occur out in the Pacific Ocean. Tsunamis have also been referred to in the past as seismic sea waves, but Earthquakes aren’t the only cause of this phenomenon. Landslides, nuclear explosions, volcanic eruptions, and extra terrestrial impacts also have great water displacement results.
The science of the natural disaster has baffled many, but from studying the San Francisco earthquake, scientists have made a number of important discoveries and they have a better understanding of earthquakes. At 5:12 on a fateful April morning in 1906, the mammoth Pacific and North American plates sheared at an incredible twenty-one feet along the San Andreas fault, surpassing the annual average of two inches (“San Francisco Earthquake of 1906”)(“The Great 1906 Earthquake and Fires”). The shearing caused a loud rumble in the Californian city of San Francisco. A few seconds later, the destructive earthquake occurred. The ground shifted at almost five feet per second, and the shaking could be felt all the way from southern Oregon to southern Los Angeles to central Nevada (“Quick”)(“The Great 1906 San Francisco Earthquake”). Moreover, the earthquake could be recorded on a seismograph in Capetown, South Africa, an astounding 10,236 miles away from San Francisco (“San Francisco ea...
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.
producing a earthquake safe environment. In a nuclear facility that in itself is a danger, an honest
Mr. Adams describes the San Francisco earthquake as his most profound human suffering experience because the horror of shaking floors, parts of his mom’s house collapse to the floor, and got a broken nose from stumbling into a brick wall (Ansel Adams & The 1906 Earthquake 2008). Earthquakes are part of natural disasters of the earth and normally caused by shaking ground and rapid movement of one block of rock slipping past another a long fractures in the earth crust called faults. Faults that are usually locked excluding abrupt movements, which slippage creates an earthquake (Lutgens, F. & Tarbuck, E.
Haiti, regarded as the second most poverty stricken country on the globe, taken in its past there is little to no uncertainty this manifested throughout years of hardship and grief. Haiti being a very new independent country in the wake of the glorious revolution did not have the easiest time. This due in great part to the colonization of Hispaniola by the french in the 17th century, where most trees were harvested for natural fuel and resources. This mass deforestation from the colonial age made is so Haiti to this day doesn't have much tree life. Soon after the French indemnity payments were done with in 1947, Haiti's economy was drained and in need of a strong leader to guide them on the right path. Haiti was appointed a new president who
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.
Where one is in the United States determines if one is in danger from a natural risk and which hazard. Some natural risks are earthquakes, tsunamis, volcanoes, hurricanes and tornadoes. Document one is a map from the natural Disaster Coalition that shows most natural risks and the areas affected in the United States. Despite showing specifically which regions are affected by certain natural risks, document one is not not complete and does not include all natural risks of the United States, leaving out certain ones like floods, wildfires, blizzards, landslides and numerous others. The west coast of the United States is prone to a lot of earthquakes. Earthquakes destroys infrastructures that leads to numerous deaths and a long recuperation periods.
In the early morning hours on January 17th, 1994 a very violent tremble took place across Los Angeles, California area that left fifty-seven people dead, more than 7,000 injured, more than 20,000 homeless and left over 40,000 buildings damaged. Around 4:30 a.m. a horrific 6.7 magnitude earthquake, that tested building codes and earthquake-resistant construction, shook Los Angeles, San Bernardino, Ventura, and Orange Counties with the most intense damage occurring in Sherman Oaks and Northridge. The earthquake caused several bridges and overpasses to collapse closing sections of the Santa Monica Freeway, Simi Valley Freeway, Golden State Freeway, and the Antelope Valley Freeway. There were also several fire outbreaks throughout the San Fernando Valley, Malibu, and Venice area because of underground gas lines that had been ruptured during the earthquake that caused additional damage.
Authorities have attempted to implement codes or regulations, but that has proved to be very difficult tasks becasue there are many variables that effect the dynamic response of buildings. One way to try to avoid disaster is to evaluate seismic risk is to look at a buildings hazards, exposure, vulnerability, and location. Hazards are, for example, landslides ad soil type. Exposure is a building's occupancy and function. Vulnerability is the expected performance of a building's system, and location is how often earthquakes occur in the area. (Lagorio)
Taher, R. (2011). General recommendations for improved building practices in earthquake and hurricane prone areas. San Francisco, CA: Architecture for Humanity Retrieved from
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).