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Term Papers on Earthquakes
Earthquakes I chose to research earthquakes and the prediction of earthquakes because I was curious as to how they work. In this paper, I will discus the history of earthquakes, the kinds and locations of earthquakes, earthquake effects, intensity scales, prediction, and my own predictions. An earthquake can be defined as vibrations produced in the earth's crust. Tectonic plates have friction between them which builds up as it tries to push away and suddenly ruptures and then rebounds. The vibrations can range from barely noticeable to a disastrous, and destructive act of nature. Six kinds of shock waves are generated in the process. Two are classified as body waves, that is, they travel through the inside of the earth and the other four are surface waves. The waves are further classified by the kinds of motions they incur to rock particles. Primary or compressional waves, known as P waves, send particles moving back and forth in the same direction as the waves are traveling, as secondary or transverse shear waves, known as S waves, create vibrations perpendicular to their direction of travel. P waves always travel at faster speeds than S waves, so whenever an earthquake occurs, P waves are the first to arrive and to be recorded at geophysical research stations worldwide. During ancient times very little was know about. Some of the ancient Greek philosophers connected earthquakes to underground winds, where others blamed them on fires in the depths of the earth. Around AD 130 the Chinese scholar Chang Heng, believing that waves must ripple through the earth from the source of an earthquake, created a bronze object to record the directions of such waves. Eight balls were carefully balanced in the mouths of eight dragons placed around the outside of the object. When a passing earthquake occurred the wave would cause one or more of the balls to drop. Earthquake waves were observed in this and other ways for centuries, but more scientific theories as to the causes of quakes were not proposed until modern times. One such concept was recreated and advanced in 1859 by an Irish engineer, Robert Mallet. Perhaps recalling on his knowledge of the strength and behavior of construction materials, Robert Mallet proposed that earthquakes occurred "either by sudden flexure and constraint of the elastic materials forming a portion of the earth's crust or by their giving way and becoming fractured." Later, in the 1870s, an English geologist, John Milne created a device similar to one of today's earthquake-recording device, a seismograph, which in Greek seismos means earthquake. A simple pendulum and needle suspended above a smoked-glass plate, it was the first instrument to allow visual difference of primary and secondary earthquake waves. The modern seismograph was invented in the early 20th century by a Russian seismologist, Prince Boris Golitzyn. His device used a magnetic pendulum suspended between the poles of an electromagnet, created the modern era of earthquake research. There are three general classes of earthquakes that are now recognized: tectonic, volcanic, and artificially produced. The tectonic kind is by far the most devastating, and these earthquakes create many difficulties for scientists trying to develop ways to predict them. The main cause of tectonic earthquakes is stress set up by movements of the dozen major and minor plates that make up the earth's crust. Most tectonic quakes occur at the boundaries of these plates, in zones where one plate slides past another, such as at the San Andreas Fault in California, North America's most quake-prone area, or where one plate slides beneath the other plate, subduction. Subduction-zone earthquakes count for nearly half of the world's destructive seismic events and 75 percent of the earth's seismic energy. They are concentrated along the "Ring of Fire", a narrow band about 38,600 km long, that meet with the border of the Pacific Ocean. The points at which rupture occurs in these earthquakes tend to be far below the earth's surface... This is ONLY a preview of the article. If you would like to view the entire document, you must subscribe to Digital Term Papers. Please register below now! Digital Term Papers has over 63,000 essays, term papers, and book notes online. Many paper sites will charge you hundreds of dollars for a single paper. Digital Term Papers only charges $14.95 for a one month membership with instant account activation! Don't waste anymore time! Join NOW!!!
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