Lecture 4 - Earthquakes, the basics Flashcards

1
Q

What is the difference between a right stepping and a left stepping right lateral fault?

A

Right stepping - The land is pulled apart at the fault bend whenever the fault moves, It creates a hole that could become a basin. Left stepping - The land is pushed together when the fault moves. Eventually could grow into a mountain

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2
Q

Where is the epicenter on the Earth’s surface?

A

Directly above the hypocenter.

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3
Q

What is the hypocenter?

A

Where the rupture began

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4
Q

Why does the epicenter not fall on the trace of the fault at the surface?

A

The dip of the fault.

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5
Q

What are the basic principles of how a seismometer works?

A
  • The earth moves moving the framework of the seismometer. - The suspended heavy weight and then pen beneath remain relatively stationary. - As the concrete base moves the stationary pen draws an ink line on paper on the rotating drum.
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6
Q

Define amplitude, wavelength and the period of waves

A
  • Amplitude: height of the waves above starting point - Wavelength: distance between successive waves - Period: time between successive waves = 1/frequency
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7
Q

Give standard strengths of body and surface waves

A

Body waves - 0.5 to 20 Hz Surface waves - 0.005 to 0.1 Hz

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8
Q

Name and describe the two types of body waves

A
  • P-waves: Travel fastest, like the push-pull motion of slinky toy (4.8km/sec in granite) - S-waves: Move in an up and down motion perpindicular to direction of advance, like the waves in a shaken rope. (3km/sec in granite)
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9
Q

What are surface waves?

A
  • Created when body waves hit surface. - They are similar to the waves created by throwing a rock into a lake
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10
Q

What kinds of waves compose the surface waves?

A
  • Love waves (horizontally polarized) and Raleigh waves (cause horizontal and vertical movement) - Travel slower than body waves but less attenuation because of long wavelength and low frequency
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11
Q

LEARN

A
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12
Q

How are earthquakes located using triangulation?

A
  • Need three seismic stations
  • Measure the P-S arrival times and convert these to distance
  • Triangulate using radius given by P-S travel times
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13
Q

Name and briefly describe the use of the three magnitude scales

A
  • Mercalli: measures damage done by an earthquake
  • Richter scale: measures the energy released during an earthquake (ML=log10A-0.15+1.6log10D) where A is the amplitude of the P-wave in mm
  • Moment magnitude (M): The seismic moment of the earthquake; the rigidity of the Earth x the amount of slip on the fault plane during the earthquake
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14
Q

Potential energy is stored in the crust in the form of built-up stress. During an earthquake, this stored energy is transformed. What does it result in?

A
  • Cracks and deformation in rocks
  • heat
  • radiated seismic energy (Es)
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15
Q

What is the seismic moment a measure of?

A

The total amount of energy that is transformed during an earthquake. Only a small fraction of the seismic moment is converted into radiated seismic energy which is what seismographs register.

This means that 99% of the energy produced by earthquakes we cannot measure!

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16
Q

Why is the moment magnitude a better measurement than the seismic moment for larger earthquakes?

A

It measures directly the amount of strain energy released by movement along rupture surface

17
Q

Why are buildings with ‘soft’ first stories especially susceptible to building damage during earthquakes?

A

No bracing on the first floor and no shear walls. Stresses are concentrated at the joints between the first and second floors. They give way causing the floor to flatten.