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
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
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
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
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
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
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
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
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
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 the lithosphere. The lithosphere is 20-50 km thick and is cracked. The asthenosphere sits below