Seismic Flashcards

(31 cards)

1
Q

What is an earthquake?

A

The shaking caused by the rupture and subsequent displacement of rocks beneath the Earth’s surface

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2
Q

What is the distribution of earthquakes?

A
  • Generally concentrated in linear clusters along plate boundaries
  • 95% occur close to or at a plate margin
  • 90% occur at the Pacific Ring of Fire
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3
Q

What is the focus of an earthquake?

A

The point at which the earthquake starts below the Earth’s surface

Shallow focus - 0-70km
Intermediate focus - 70-300km
Deep focus - 300-700km

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4
Q

What is the epicentre of an earthquake?

A

The point on the Earth’s surface where seismic waves reach first - usually above the focus

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5
Q

How do earthquakes form?

A
  • Tectonic plates move due to convection currents and processes like slab pull and ridge push
  • Plates become stuck due to friction between plates
  • This causes rocks to deform which leads to a build up of stress and pressure
  • When the rock can no longer stand the deformation, it fractures and the two sides slide past each other
  • This releases energy in a process known as elastic rebound
  • Seismic waves travel outward from the focus towards the Earth’s surface, causing the ground to shake
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6
Q

What is an aftershock?

A

An earthquake triggered by stress transfer from a preceding earthquake

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7
Q

What are the different types of shockwaves?

A

Body - P waves, S waves
Surface - L waves, R waves

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8
Q

What are P (primary) waves?

A
  • Fastest, reach surface first
  • Travel through solids and liquids (mantle and core)
  • Longitudinal
  • Least damaging
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9
Q

What are S (secondary) waves?

A
  • Half as fast as P waves
  • Reach surface 2nd
  • Only travel through solids (mantle)
  • Transverse
  • More damaging than P waves
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10
Q

What are L (love) waves?

A
  • Slowest
  • Cause most damage
  • Transverse
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11
Q

What are R (Rayleigh) waves?

A
  • Longitudinal
  • Radiate from the epicentre in a complicated low frequency rolling motion
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12
Q

How is magnitude measured?

A

From the epicentre using seismographs

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13
Q

What scales are there to measure earthquakes?

A
  • Richter scale
  • Moment magnitude scale
  • Modified mercalli scale
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14
Q

What is classified as a major earthquake?

A

Magnitude greater than 7

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15
Q

Outline the frequency and regularity of earthquakes

A
  • Low frequency EQs occur much more frequently than high magnitude
  • 20,000 every year
  • 55 per day
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16
Q

Can earthquakes be predicted?

A

No, but plate tectonics show areas where EQs are most likely to occur

17
Q

What are signs before an earthquake?

A
  • Microquakes, bulging of ground
  • Decreasing radon gas concentration in groundwater
  • Raise groundwater levels
  • Electric and magnetic charges within local rocks
  • Curious animal behaviour
18
Q

Outline liquefaction

A

Liquefaction is when saturated, loose soil temporarily loses its strength and behaves like a liquid

If soil is saturated, shaking causes the liquid to move into gaps between the soil grains - pore spaces. This causes the soil particles to lose contact with each other, decreasing the overall strength of the ground.At the same time, the water is responding to the increase pressure by trying to move up towards the surface. The sediments lose their structure and therefore strength, acting as a liquid when the ground begins to shake. Can cause buildings and infrastructure to collapse.

19
Q

What is a landslide (with example)?

A

The downward movement of soil and rock on a slope. Occurs due to intense shaking cause the collapse of material downhill.

eg. 2008 Sichaun Earthquake caused 60,000 landslides

20
Q

What is a tsunami?

A

Tsunamis are giant waves caused by earthquakes or volcanic eruptions under the sea

21
Q

How are tsunamis formed?

A
  • When oceanic crust is jolted during an earthquake, all of the water above the plate is displaced and forced upwards, creating a wave
  • This water travels fast at a low amplitude
  • As it approaches the coast, the sea level decreases so there is friction between the sea bed and waves
  • This causes the waves to slow down and gain height
22
Q

Outline the 2011 Tohoku Earthquake and Tsunami

A
  • Magnitude of 9.0
  • Depth of 30km
  • Occurred 400km off the North-East coast of Japan
  • Tsunami waves reached up to 40m
  • At destructive boundary where the Pacific Plate subducts the North American Plate
23
Q

What were the primary impacts of the 2011 Tohoku Earthquake and Tsunami?

A
  • Over 15,000 deaths, over 90% due to drowning
  • Over 1 million buildings damaged
  • Sendai City was completed flooded, leaving many without electricity, water and communication systems
  • $235 billion in economic losses -> most expensive natural disaster in history
  • Saltwater damaged crops and soils
24
Q

What were the secondary impacts of the 2011 Tohoku Earthquake and Tsunami?

A
  • 240,000 still living in temporary housing 3 years later
  • 600 factories shut, causing Japan’s industrial production to fall by 15%
  • Disabled cooling systems of 3 nuclear reactors, leading to core meltdowns -> 520km^2 of land around Fukushima was contaminated by radioactive fallout
  • Liquefaction destroyed over 1000 buildings in Tokyo
25
What were the immediate responses to the 2011 Tohoku Earthquake and Tsunami?
- 1.5 million food rations delivered in the first few days by the Japanese Red Cross society - 1 million households had access to water restored after 2 weeks - 470,000 evacuated in 2500 evacuation centres - 100,000 of the Japanese Self-Defence Forces deployed for search and rescue - Over 25 search and rescue teams from 20 countries - Over 380 medical teams
26
What were the long-term responses to the 2011 Tohoku Earthquake and Tsunami?
- New housing developments constructed on higher ground to reduce future risk - Government launched a reconstruction programme worth over £200 billion -> over 400km of roads and railways rebuilt, 15 major ports reconstructed - New tsunami sea walls up to 15m high built along the northeast coast
27
What is the potential mega-tsunami?
- Scientists said that an eruption of the Cumbre Vieja volcano in the Canary Islands cold cause a huge chunk of the volcano's western flank to collapse into the Atlantic - Could cause waves to reach Europe, Africa and the Carribean - However, scientists now believe this is unlikely
28
Outline monitoring during the 2011 Tohoku Earthquake and Tsunami
- 11-12 GPS buoys which allowed authorities to update warnings quickly - 50 DART (Deep-ocean Assessment and Reporting of Tsunamis) Buoys helped track the tsunami across the Pacific - 1000+ seismometers nationwide gave immediate estimation of location, depth and magnitude
29
Outline prediction during the 2011 Tohoku Earthquake and Tsunami
- JMA used a database of 100,000+ tsunami simulations but wave height was severely underestimated (5 vs 40m) - Long term hazard mapping identified the Japan Trench as high risk
30
Outline protection during the 2011 Tohoku Earthquake and Tsunami
- Strict seismic building codes including flexible steel frames - 80% of urban residential buildings are now earthquake resistant - Sea walls overtopped
31
Outline planning during the 2011 Tohoku Earthquake and Tsunami
- 80-90% of coastal municipalities had tsunami hazard maps - Regular drills on Disaster Prevention Day (1st September)