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Published byAdele Mills Modified over 8 years ago
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earthquake: shaking and trembling that results from sudden movement of part of the Earth’s crust Caused by release of energy (lithospheric plates)
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OCCURS FOR MANY REASONS: ground shakes from erupting volcano collapse of a cavern impact of meteor major cause- stress that builds up and causes faulting
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Elastic rebound theory: rocks that are strained past a certain point will fracture and spring back to their original shape
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Depth inside the Earth at which an earthquake occurs depends upon the kind of plate boundary focus: point beneath the Earth’s surface where the rocks break or move apart Point on fault plane where 1 st movement occurs
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epicenter: point on Earth’s surface directly above the focus site of most violent shaking focus
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P waves (primary): move fastest back and forth waves move through solid, liquid or gas push-pull waves
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S waves (secondary): travel slower move side to side travel through solids
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L waves (surface): move slowest move like ripples on a pond
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Blue primary waves followed by red secondary waves move outward in concentric circles from the epicenter of an earthquake off British Columbia and Washington State.
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Seismograph: instrument that detects and measures seismic waves
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Seismogram:seismograph’s record of waves; has wavy lines recorded on paper
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Seismogram
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Seismologist: scientists who study earthquakes
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Tracing made by a seismograph can be used to tell how far away an earthquake’s epicenter is from the station that recorded it: Need distance from 3 different stations in order to determine location Point where all 3 circles meet is location of epicenter
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Locating an Earthquake
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seismograms can be used to determine strength or magnitude of energy produced by an earthquake Richter scale: measures how much energy an earthquake releases by assigning a number from 1 to 10- each is 10x’s higher
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Pacific Ring of Fire: major earthquake zone that forms a ring around the Pacific Ocean
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Successful earthquake prediction must correctly forecast: where it will occur when it will occur what magnitude it will be
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Possible methods for prediction: detect slight tilting of ground before an earthquake natural gas seepage Microquakes (foreshocks)
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Foreshocks & Aftershocks Foreshock: small earthquakes that occur prior to a major quake Aftershock: small earthquakes generated by adjustments of materials that follow a major quake.
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Animal Behavior Unusual behavior prior to an earthquake event behavior of animals 2004 Indonesia Tsunami –In Thailand, elephants broke their chains and ran to a mountaintop –People survived by following animals (monkeys, elephants, dolphins) fleeing from the coast. –Very few animal corpses were found
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Fault Fractures in the Earth where movement has occurred. Causes by stress
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faulted rocks have two blocks: –hanging wall: block of rock above fault –foot wall: block of rock below fault
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Types of Faults normal fault : formed when hanging wall moves down relative to the foot wall
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reverse fault : formed when hanging wall moves up relative to the foot wall
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strike-slip fault : rocks on either side of fault are moving past each other
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fold : bend in the rock (rock deformed but doesn’t break) anticline: upward fold in the rock (forms ridges) syncline: downward fold in the rock (forms valleys)
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