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Earthquake Properties http://www.worldphoto360.com/wp-content/uploads/2009/12/Earthquake.jpg Slide 2 Physical Properties Focus point of rock failure where the earthquake originates Epicenter - The point on the earth's surface directly above the earthquake's focus Slide 3 Seismic Waves Vibrations generated during an earthquake Slide 4 Types of Earthquake Waves Surface waves Travel on Earths surface outward from the epicenter in a circular motion pattern Complex motion Slowest velocity of all waves Slide 5 Types of Earthquake Waves Body waves - travel through interior of Earth 1. Primary (P) waves Push-pull (compressional) motion Travel through solids, liquids, and gases Greatest velocity of all earthquake waves Slide 6 Types of Earthquake Waves Body waves - travel through interior of Earth 2. Secondary (S) waves "Shake" motion Travel only through solids Slower velocity than P waves Slide 7 A seismogram records wave amplitude vs. time http://ww2.lafayette.edu/~malincol/Geol120/seismogram.GIF Slide 8 The machine that produces seismograms is called a seismograph. http://upload.wikimedia.org/wikipedia/commons/0/0f/Kinemetrics_seismograph.jpg http://www.cartage.org.lb/en/themes/Sciences/Earthscience/Geology/Earthquakes/Mea suringEarthquakes/Seismographs/seismograph.GIF Slide 9 Locating an epicenter requires 3 seismograph stations. Slide 10 Distance from the epicenter to a station is determined by the difference in arrival time between P and S waves. Slide 11 Calculate distances from 3 stations and see where the circles intersect. 300 km 500 km 100 km Slide 12 Measuring The Size of An Earthquake Intensity qualitative; determined by effects on people, structures, and the environment Magnitude quantitative; measures energy released at the source of the earthquake Slide 13 Magnitude Scales Richter scale - measures earthquake magnitude based on size of largest wave Moment magnitude scale - accounts for size of fault rupture, amount of movement at fault, and rocks stiffness more precise Each step represents a 10-fold increase in wave size, or a 30-fold increase in energy released A magnitude 6 earthquake is 10 times bigger than a magnitude 5 earthquake and releases 30 times more energy. A magnitude 7 earthquake is 100 times bigger than a magnitude 5 earthquake and releases 900 times more energy. Slide 14 Slide 15 Moment Magnitude Moment = A D = shear modulus A = LW = area D = average displacement during rupture Source: USGS The seismic moment is a measure of the size of an earthquake based on the area of fault rupture, the average amount of slip, and the force that was required to overcome the friction sticking the rocks together that were offset by faulting. slip Slide 16 Magnitude From Amplitude http://www.earthquakes.bgs.ac.uk/earthquakes/education/eq_booklet/dia_richter_scale.jpg Slide 17 Lets try it! An earthquake has been recorded on 3 seismograms. Can you locate its epicenter? Can you determine its magnitude? http://www.divinationpower.com/UserFiles/2009/12/1/Earthquake%20measuring%203.7%20in%20magnitude%20jolts%20northeastern%20Bulgaria.jpg Slide 18 Intensity Witness observations I Felt by very few people; barely noticeable II Felt by a few people, especially on upper floors. III Noticeable indoors, especially on upper floors, but may not be recognized as an earthquake. Hanging objects swing. IV Felt by many indoors, by few outdoors. May give the impression of a heavy truck passing by. V Felt by almost everyone, some people awakened. Small objects move. Trees and poles may shake. VI Felt by everyone. Difficult to stand. Some heavy items of furniture move, plaster falls. Slight damage to chimneys possible. VII Slight to moderate damage in well-built, ordinary structures. Considerable damage to poorly built structures. Some walls may fall. VIII Little damage in specially built structures. Considerable damage to ordinary buildings, severe damage to poorly built structures. Some walls collapse. IX Considerable damage to specially built structures, buildings shifted off foundations. Noticeable cracks in ground. Wholesale destruction. Landslides. X Most masonry and frame structures and their foundations destroyed. Ground badly cracked. Landslides. Wholesale destruction. XI Total damage. Few, if any, structures standing. Bridges destroyed. Wide cracks in ground. Waves seen on ground. XII Total damage. Waves seen on ground. Objects thrown up into air. Abbreviated Modified Mercalli Intensity Scale Slide 19 Slide 20 Intensity Intensity when focus depth Intensity when distance from epicenter Also depends on what ground is made of why? Lets see it! Slide 21 http://earthquake.usgs.gov/eqcenter/dyfi.php Did You Feel It?