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Warmup 1. What is an earthquake’s location on a surface called?
2. What is an earthquake’s location underground called?
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7.3 Earthquakes
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Earthquakes Earthquake- The shaking of the Earth’s crust cause by rapid displacement of rocks, usually along a fault.
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Epicenter- the point on the Earth’s surface directly above the focus of an earthquake.
Focus- the point within the crust where an earthquake originates
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Earthquake Waves
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Body Waves P-waves (primary or push-pull waves)- they cause back-and- forth motion in the same direction as the wave is traveling S-waves (secondary or shear waves)- they cause motion at right angles to the direction in which the wave is traveling
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Surface Waves L-Waves (love or long waves)- travel along the Earth’s surface at slow speeds back and forth R-Waves (Rayleigh waves)- travel along the Earth’s surface similar to an ocean wave
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Measuring Earthquakes
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Seismic Waves- energy waves set in motion by an earthquake
Seismograph- an instrument used to record seismic waves
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Paths of Body Waves P-waves travel faster than S- waves
Seismic waves travel faster through denser materials Seismic wave bend (refract) as they move from a medium of one density into a medium of a different density S-Waves will not travel through Earth’s outer core (which is liquid)
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Earthquake Strength
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Locating Epicenters Find difference in travel time between P and S Waves Use table to determine “distance from epicenter” for 3 seismograph stations Epicenter is located where 3 circles intersect
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Faults Compression – the type of stress that occurs when an object is squeezed, such as when 2 tectonic plates collide. Tension- the force (stress) that occurs when forces act to stretch an object.
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Folding- the bending of rock layers due to stress
Two main types of folds: Anticlines- upward arching folds Synclines- downward troughlike folds
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Fault- the surface along which rocks break and slide past one another.
2 Main types of faults: Normal faults- occur at divergent boundaries Reverse faults- occur at convergent boundaries
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