Lecture 7: Seismic Waves and EQs Flashcards

1
Q

Strike

A

Azimuth or bearing of a horizontal line in the plane

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2
Q

Dip

A

The slope of the plane in the direction perpendicular to strike

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3
Q

Fractures

A

Break in rocks or sediments

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4
Q

Faults

A

Fractures that have motion (slip, displacement) along them in some direction

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5
Q

Fault plane

A

The plane of the fracture; not usually an flat surface, but curved or irregular

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6
Q

Hypocenter

A

Where on the fault plane the rupture began (in seconds it can travel over a larger area)

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7
Q

Epicenter

A

The location on the Earth’s surface projected directly above the hypocentre

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8
Q

Seismic

A

Related to EQ

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9
Q

Seismograph

A

Instrument that records vibrations Need one in every direction

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10
Q

Seismogram

A

Record of vibrations recorded by seismograph

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11
Q

Seismic wave

A

Any of the waves that are generated by an earthquake

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12
Q

Seismic moment

A

Direct measure of the energy radiated during an EQ A measure of the size of an earthquake based on the area of fault rupture, the average amount of slip, and the force that was required to overcome the friction sticking the rocks together that were offset by faulting Moment = shear modulus x area of rupture x average displacement during rupture

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13
Q

S waves

A

Secondary waves, slower

Increases velocity and decreases amplitude

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14
Q

P waves

A

Primary waves

Can be felt by animals

Increases velocity and decreases amplitude

Use difference between arrival of P and S wave to determine how far away EQ is

Compression waves

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15
Q

Surface waves

A

Constant velocity

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16
Q

How to locate epicenter

A

Need 3 seismometers Triangulate position of epicenter and focus

17
Q

Richter scale

A

Used for local EQ only

18
Q

Using seismogram to determine dip slip fault

A

Will see either initial pull down, or push up depending on what size of fault seismograph is on

19
Q

Body waves

A

P and S waves Traveling through the interior of the earth, body waves arrive before the surface waves emitted by an earthquake. These waves are of a higher frequency than surface waves

20
Q

Surface waves

A

Travelling only through the crust, surface waves are of a lower frequency than body waves, and are easily distinguished on a seismogram as a result. Though they arrive after body waves, it is surface waves that are almost enitrely responsible for the damage and destruction associated with earthquakes. This damage and the strength of the surface waves are reduced in deeper earthquakes

21
Q
A

Normal fault

22
Q
A

Reverse fault

23
Q
A

Strike-slip fault