Josh Sharma NSCI 115 Prof. Anglen March 15, 2009 EARTH TREMORS Josh Sharma ABSTRACT reasonquakes argon an Brobdingnagian phenomenon that we experience e'ery so often on Earth. in that respect’s no exact science on how to retire when an earthquake will happen. You just never know, it could happen in a twosome of months, or even a couple of hundred years. There just is not a kick and precise way to predict these phenomena. All you can do is make a “forecast†of where an earthquake could take place, found on probabilities and old shift key lines and systems. INTRODUCTION An earthquake is a choppy release of energy in Earth’s encrustation that creates unstable waves. Most earthquakes occur on faults in the Earth’s crust. The epicenter is the point on ground take that earthquake is projected to have occurred. The focus is where the energy is released; it’s initial rupture. Earthquakes occur when two different tectonic plates chafe on for each one other, causing strain and built up energy. They occur when the two tectonic plates “have had enough†and seismic waves are released. There are several different types of seismic waves that spread out through the earth’s surface. lieu or predicting earthquakes is the hardest part of figuring out how earthquakes work.
DISCUSSION There are a few different types of faults that earthquakes occur at. There is a normal fault, which is a dip-slip of the fault. This type of fault occurs in reply to extension and is commonly found on the west brim of California. In California, we have a fault line that runs in all the way down California. It is predicted that San Francisco and Los Angeles will be adjacent to each other in 15 million years. The plates are wretched at the speed our finger nails are growing ever two years. The second fault is the thrust fault, which is a dip-sip fault where one plates thrusts on top of the lower plate. This type of faulting is more often than not common in places where a lot of compression is present, usually where one plate is being... If you want to get a all-embracing essay, order it on our website: Orderessay
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DISCUSSION There are a few different types of faults that earthquakes occur at. There is a normal fault, which is a dip-slip of the fault. This type of fault occurs in reply to extension and is commonly found on the west brim of California. In California, we have a fault line that runs in all the way down California. It is predicted that San Francisco and Los Angeles will be adjacent to each other in 15 million years. The plates are wretched at the speed our finger nails are growing ever two years. The second fault is the thrust fault, which is a dip-sip fault where one plates thrusts on top of the lower plate. This type of faulting is more often than not common in places where a lot of compression is present, usually where one plate is being... If you want to get a all-embracing essay, order it on our website: Orderessay
Order your essay at Orderessay and get a 100% original and high-quality custom paper within the required time frame.
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