Lecture 3 - Earthquakes and Volcanoes Flashcards

1
Q

What is the most common reason for an earthquake?

A

Movement of the plates

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2
Q

Epicentre?

A

The point where the seismic rupture begins (origin)

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3
Q

Seismograph?

A

Used to measure an earthquake

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4
Q

Earthquake magnitude?

A

Measured by moment magnitude, logarithmic, quantitative measurement (M1, M5, etc.)

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5
Q

Earthquake intensity?

A

Modified Mercalli intensity scale: qualitative, based on damage to structures/perceptions (I - XII)

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6
Q

Shake maps?

A

Use seismograph data to show areas of intesnes shaking

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7
Q

Dip slip fault?

A

Vertical movement, includes Normal, Reverse, and Blind

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8
Q

Hanging wall?

A

The top wall of a fault

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9
Q

Footwall block?

A

The bottom wall of a fault

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10
Q

Normal fault?

A

The hanging wall moves down

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11
Q

Reverse fault?

A

The hanging wall moves up

thrust fault: if a reverse fault is 45º or less

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12
Q

Blind fault?

A

Don’t extend to the surface

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13
Q

Strike slip fault?

A

Horizontal movement: the plates slide past eachother

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14
Q

Active fault:

A

movement during the past 11 600 years

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15
Q

Potntially active fault:

A

movement during the past 2.6 million years

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16
Q

Inactive fault:

A

no movement in the last 2.6 million years

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17
Q

Tectonic creep?

A

Movement along a fault is so gradual that earthquakes are not felt

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18
Q

P waves (primary/compressional)?

A

move fast with a push/pull slinky motion, good in all states of matter

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19
Q

S waves (secondary/shear?)

A

moves like a water wave, but only through solids

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20
Q

Surface waves?

A

rolling waves on the surface that move more slowly than body waves

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21
Q

Love waves

A

surface waves that cause horizontal shaking

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22
Q

Rayleigh waves

A

surface waves with rolling motion

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23
Q

How can distance to the epicentre be determine from S and P waves?

A

Compare travel times of the two wave types using triangulation

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24
Q

When does amplification occur?

A

When energy is transferred from P and S waves to surface waves

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25
What are the steps of the earthquake cycle?
- inactive period (stress builds) - foreshock (occur prior to major release) - main shock (majority of the stress is released) - aftershock (releases of stress after major earthquake)
26
Intraplate Earthquakes?
Occur within plates, not at a boundary | - often smaller than plate boundary earthquakes
27
Precursor?
An event that signals that an earthquake may be imminent - pattern/freq of earthquakes - land level change (uplift/subsidence) - seismic gaps (haven't seen an earthquake in a while) - physical/chemical changes
28
How much time does the current warning system give for an earthquake?
15s to one minute
29
Where are 2/3 of all active land volcanoes found?
Pacific Ring of Fire
30
Magma
molten rock
31
Lava?
magma that reaches the earth's surface
32
Pyroclastic debris?
Leava and rock fragments ejected in a volcanic eruption
33
Volcano?
hill or mountain produced by volcanism
34
Vent?
opening through which eruption akes place
35
Crater?
depression over the vent
36
Caldera?
a depression over 1km wide
37
Where does most magma come from?
Asthenosphere
38
Decompression
Magma is formed - pressure on hot rock is reduced
39
Addition of volatiles
Magma is formed - chemcial compounds lower the melting temp of the rock
40
Addition of heat
Magma is formed - heat overlying rocks as magmas rise
41
What are the two most abundant elements in magma
Silica and Oxygen - SiO2
42
Silica-Rich (felsic) Lavas
Very viscous, flow slowly - violent explosive eruptions - rhyolite
43
Silica-Poor (mafic) lavas
Low viscosity, flow easily, quiet eruptions/lava flows | - basalt
44
Intermediate lavas
Andesite
45
Shield Volcanoes
- largest volcanos in the world - arch/dome - low silica (mafic) lava - basalt - not too explosive - mauna loa (hawaii)
46
Composite Volcanoes
- Cone shaped - intermediate lava, high silica but low viscosity - andesite (dicitic) - lava flows and explosive activity - volcan osorno, chile
47
Volcanic Domes
- dome shaped - high silica (felsic) magma - very explosive - rhyolite - mono craters, california
48
Cinder Cone Volcanoes
- steep cone - low silica (mafic) magma - not very explosive - basalt - mount edziza, BC
49
Maars?
The interaction of magma and groundwater: produces roughly circular craters filled with water
50
Ice Contact Volcanoes
Erupt beneath or against glaciers
51
Jokulhaups
Huge floods produced from subglacial volcanoes
52
Hot springs
hot rocks heat grounwater that discharges at the surface
53
Geysers
Groundwater boils an underground chamber, erupting steam at the surface
54
Resurgent Calderas and super eruptions
very rare but very violent eruptions from supervolcanoes
55
Highest mountain in canada?
mt logan
56
Volcano that poses the biggest threat to Canada?
Mt baker in washington
57
What are some primary effects of a volcano?
Lava flows, ash fall, volcanic bombs, pyroclastic flows, pyroclastic surges, lateral blasts, poisonous gases
58
Secondary effects of a volcanic eruption?
Lahars (mudflow), debris avalanches, landslides, groundwater/surface contamination, floods, fires, tsunamis
59
Two types of balsaltic lava flows?
Pahoehoe (smooth ropy texture, faster) | Aa (more viscious, more damaging, slow)
60
Sector Collapse
the flank of a volcano may collapse due to shaking
61
Mt St Helens
``` May 1, 1980, a large bulge began to grow May 18, a M5.1 earthquake triggers a landslide/debris avalanche Seconds later, a LATERAL BLAST Cloud of ash Mudflows (Lahars) 57 People Killed ```
62
How can we manage volcanoes?
- Bombing (block channels to cause lava flows to take a dif route) - Hydraulic Chilling (water) - Wall construction