GENERAL GEOLOGY (EQUAKE) Flashcards

1
Q

catastrophic magnitude 7.0 Mw earthquake struck

A

January 12 2010

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2
Q

Epicenter of such earthquake

A

25 km of Port-au-Prince

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3
Q

Depth

A

10km

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4
Q

Ground shaking caused by sudden rapid omvement of one block of rock slipping past another along factures in earth’s crust

A

Earthquake

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5
Q

Fractures on Earth’s crust which are locked due to the enormous confining pressure exerte by the overlaying crust except for brief abrupt movements when sudden slippage

A

Faults

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6
Q

The location where slippage of fault begins

A

hypocenter or focus

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7
Q

The point on earth’s surface directly above the focus

A

epicenter

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8
Q

A form of energy that travels through the lithosphere and earth’s interior that causes the material that transmit such energy to shake

A

Seismic Waves

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9
Q

How many strong equakes mag 7 or greater happen every year?

A

15

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10
Q

Who first studied the actual mechanism of earthquake generation

A

H.F. Reid from John Hopkins University

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11
Q

What earthquake served as the model of such study

A

1906 San Fancisco Earthquake

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12
Q

What fault moved in the said earthquake

A

San Andres Fault

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13
Q

What plates moved?

A

Pacific and N. American

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14
Q

Earthquake generation according to Reid

A

1) Differential stress due to tectonic plates movement slowly bends crustal rocks on both sides
2) Once strength of rocks is exceeded, slippage occur along the fault to produce equake
3) The rocks return to their original shape but in a new location

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15
Q

this prevents the fault from fracturing and slipping

A

Frictional Resistance

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16
Q

How is friction enhanced?

A

Irregularities that occur along fault surface

17
Q

The springing back of rock to its original, stress-free shape after slippage

A

Elastic Rebound

18
Q

Lesser magnitude quakes that follow a large equakes due to the crust along the fault surface adjusting to the displacement caused by the main shock

A

Aftershocks

19
Q

.

A

Foreshocks

20
Q

theory wc states that large slabs of Earth’s lithosphere are continually grinding past one another

A

Plate tectonics

21
Q

Seismometer

A

Instrument that record vibration

22
Q

Seismograph

A

Resulting graph

23
Q

Body waves

A

Emanate from the focus and travel in all direction through the body of the Earth

24
Q

P wave

A

?Compressing and expanding movemnt
?Depends on the incompressibility (Bulk’s Modulus) and Rigidity (Shear Modulus)
?HIghestVelocity and will always reach seismographs first

25
Q

S Wave

A

?Perpendicular shearing movement to the direction of the wave
?Depends on the resistance to shearing of a material (rigidity)
?Will always arrive second to Pwave

26
Q

Surface Waves

A

?Do not travel through the Earth
?Travel along paths that are parallel to the Surface of the Earth
?Slower than S waves

27
Q

Love Waves

A

?Side to Side perpendicular to wave direction

28
Q

Rayleigh Waves

A

?Counterclockwise eliptical up and down

29
Q

P-wave ShadowZone

A

Zone on the opposite side of earth from an earth focus that receive NO WAVES because waves are REFRACTED INWARD due to sudden decrease in velocity of Pwave at the boundary

30
Q

S-wave shadow Zone

A

Zone on the opposite side of Earth from the focus where there is no S-wave reaching the area due to non passing of S-wave through the core