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Published byAmos Lambert Modified over 5 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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Causes of earthquakes:
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 NOT spring back to their original shape
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focus: point beneath the Earth’s surface where the rocks break or move apart
Point on fault plane where 1st movement occurs
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epicenter: point on Earth’s surface directly above the focus
site of most violent shaking
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How deep in the Earth an earthquake occurs depends on the kind of plate boundary
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Types of Seismic Waves:
P waves (primary): move fastest back and forth waves move through solid, liquid or gas push-pull waves
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Types of Seismic Waves:
S waves (secondary): travel slower move up and down travel through solids ONLY
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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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Measuring Earthquakes
Earthquake Distance • The epicenter is located using the difference in the arrival times between P and S wave recordings, which are related to distance.
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Earthquake Distance
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Measuring Earthquakes
Earthquake Strength • Magnitude- amount of energy released at the earthquakes epicenter Richter scale: measures how much energy an earthquake releases by assigning a number from 1 to 10
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Earthquake Strength
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Measuring Earthquakes
Earthquake Strength • Intensity- effect of an earthquake on the Earth's surface Mercalli Scale: measures the effect of an earthquake; scale based on how the effects of an earthquake are felt
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Earthquake Direction
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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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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Locating an Earthquake
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Some Notable Earthquakes
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Pacific Ring of Fire: major earthquake zone that forms a ring around the Pacific Ocean
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Indian Ocean Earthquake
December 26, 2004
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Earthquakes May Cause... Building collapse Landslides Fire
Liquefaction Tsunamis
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Liquefaction conversion of soil into a fluidlike mass during an earthquake or seismic event Liquefaction Animation
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Tsunami Extremely large ocean wave caused by an earthquake on or near the ocean floor
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Tsunami
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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:
microquakes behavior of animals detect slight tilting of ground before an earthquake natural gas seepage
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