Thursday, March 14, 2019

Earthquakes: Application of Mathematics Essay example -- Geology

Earthquakes An Application of MathematicsThe October 13, 2010 quake triggered a large bombination across okay Universitys Norman campus, startling students walking to crystalize or sitting in the middle of calculus. This magnitude 4.3 earthquake was 10 miles southeast of Norman and was felt as far north as Stillwater. To many students, the few seconds of shaking was unrecognizable as an earthquake because okays seismicity is not well known. In reality, Oklahoma experiences multiple earthquakes, more or less daily they be usually just not strong generous to be felt. While understanding how and why earthquakes occur in Oklahoma involves knowledge of faults and rock types, the methods involved in locating the epicenter of an earthquake and find its magnitude require an awareness of the mathematical principles involved The revolve about of an earthquake is the spot within the earth where the earthquake originates, where the fault is initiative ruptured. The epicenter of a n earthquake is the location on the earths show up directly above the focus. When attempting to locate the epicenter of an earthquake, an understanding of seismic waves is crucial. on that point are ii types of seismic waves, body waves and start waves. Love and capital of North Carolina waves are surface waves that travel across the earths surface and are responsible for a majority of the shaking felt during an earthquake. The two types of body waves, p and s-waves are more useful in determining information about earthquakes. Body waves travel throughout the interior of the earth, propagating from the focus of the earthquake eventually reaching seismograph stations. The arrival times of p and s-waves are used to locate the epicenter of the earthquake as the waves are put down onto ... ...here are debates about which scale is the most precise, although most seismologists claim the atomic number 42 magnitude scale to be the most consistently accurate. Works Cited http//eqs eis.geosc.psu.edu/cammon/ hypertext mark-up language/Classes/IntroQuakes/Notes/waves_and_interior.html http//eqseis.geosc.psu.edu/cammon/HTML/Classes/IntroQuakes/Notes/waves_and_interior.html http//www.tulane.edu/sanelson/geol204/eqcauses.htm http//www.tulane.edu/sanelson/geol204/eqcauses.htm http//earthquake.usgs.gov/ see/topics/measure.php http//earthquake.usgs.gov/learn/topics/measure.php http//earthquake.usgs.gov/learn/topics/richter.php http//earthquake.usgs.gov/learn/topics/measure.php http//earthquake.usgs.gov/learn/topics/measure.php http//earthquake.usgs.gov/learn/topics/measure.php http//www.okgeosurvey1.gov/media/Oct13-2010-FactSheet_Revision2.pdf

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