Lecture 1 Flashcards

1
Q

What is the lithosphere made up of

A

Crust, Moho, Upper Mantle

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2
Q

Definition of Seismic Waves

A

Parcels of elastic strain energy that propagate outwards from a seismic source

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3
Q

What does seismic velocity depend on?

A

Velocities depend strongly on the elastic properties and the density of the rock that the seismic wave is travelling through

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4
Q

Define potential fields

A

The study of the earth gravity and magnetic fields and their perturbations at the Earth’s surface

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5
Q

Name what the Earth’s interior is made up of

A
Crust
Moho
Upper Mantle 
Lower Mantle 
“D” layer - discovered from seismology 
Outer core - elastic, propagates elastic waves
Solid-Liquid boundary 
Inner Core -more elastic
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6
Q

Geophysical rock properties

A

Density
Theological
Thermal conductivity
Magnetic properties

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7
Q

How many seismometers are used when recording earthquakes

A

3

Records N/S, E/W and up and down.

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8
Q

Larger seismometers record what

A

Higher waves

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9
Q

Smaller seismometers record what

A

Lower waves

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10
Q

Broadband seismometers

A

Get large range of frequencies

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11
Q

Type of Seismic Waves

A

Body Waves:

  • Primary Wave
  • Secondary Wave

Surface Waves:

  • love wave
  • Rayleigh wave
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12
Q

Can S waves propagate through fluids?

A

No

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13
Q

Define Epicentre

A

The point on the Earth’s surface that is directly above the the hypocentre where the earthquake begins

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14
Q

Define Hypocentre

A

The point within the Earth’s interior where an earthquake originates

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15
Q

PREM

A

Preliminary Reference Earth Model

One dimensional model representing the average Earth properties as a function of planetary radius

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16
Q

Why does the crust-Mantle boundary have such a large velocity change?

A

Due to the litho and asthenosphere boundary

17
Q

How thick is the Moho

A

30-45Km

18
Q

Passive Seismology Definition

A

Recording earthquakes caused by nature

19
Q

Active Seismology

A

Actively producing your own seismic wave source