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EOSC 114 EARTHQUAKES LEARNING OBJECTIVES QUESTIONS WITH COMPLETE ANSWERS..

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EOSC 114 EARTHQUAKES LEARNING OBJECTIVES QUESTIONS WITH COMPLETE ANSWERS

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How do we learn about ground shaking?


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- eyewitness
- measuring movement (Accelerograph = records the change in
acceleration of the ground, responds to much larger variations of motion
than seisomenter)




Describe how an earthquake is recorded and how to locate the epicentre.


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, Seismogram: a graph that plots ground motion in relation to time,
produced by a SEISMOMETER (pendulum seismometer)


Pendulum Seismometer: a heavy mass with a spring is attached to a pen,
and as the ground moves the paper moves but the mass remains constant
(new seismometers record velocity vs. time)


To locate an Epicentre: Set up 3 seismometers and see how often they
receive waves and calculate the distance and outline the circle where the
earthquake location could be -wherever the circles intersect is where the
epicentre is locate

Method: P-waves travel faster than S-waves, a bigger difference means the
location is farther apart


distance = (Time of S - Time of P)/((1/Velocity of S)-(1/Velocity of P))

-Accelerograph = records the change in acceleration of the ground,
responds to much larger variations of motion than seisomenter




Explain factors that determine earthquake intensity.


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1. Earthquake magnitude: cause them to be stronger, and more
catastrophic

2. Duration of Shaking: longer duration, causes more damage

3. Distance of Epicentre: closer to the epicentre, more intense


4. Ground Type: waves travel faster and are more intense in hard rock




What are the different types of forces that affect plates?

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compressional forces - those that cause squeezing (convergent)
tensional forces - those that cause a pulling apart of material (divergent)
shear forces- those that cause twisting or shearing (transform)




Describe the global distribution of earthquakes and how often quakes of various
magnitudes occur.


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- Global distribution: primarily at plate boundaries, with the largest
happening at collision zones (such as subduction zones)
- margin of Earth's tectonic plates


•Most earthquakes occur in specific areas, but there are a few single ones
that don't follow the pattern = earthquakes do not occur with equal
likelihood everywhere.
- largest EG's have all occurred on the edges where continents meet
oceans

Earthquakes of large magnitudes occur less frequently than smaller
magnitude earthquakes.




Where are EQ's the largest?


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- near/on subduction zones

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