Seismic Hazards Flashcards

(37 cards)

1
Q

Explain how an earthquake occurs in 6 steps?

A
  • Earthquakes occur due to stress release along faults caused by plate movements.
  • The focus is the point underground where the earthquake starts.
  • The epicentre is the point directly above the focus on the surface.
  • Large amounts of energy are released.
  • Much of this energy is transferred vertically to the surface and then moves outwards from the epicentre (point on surface above the focus) as seismic waves
  • After the moment of fracture, rocks may regain their original shape but in a new position.
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2
Q

What are the 2 primary hazards of earthquakes?

A
  • Ground shaking: Causes buildings to collapse.
  • Crustal fracturing: The Earth can visibly separate and deep fissures in the ground can be created.
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3
Q

What are the 3 secondary hazards of earthquakes?

A
  • Liquefaction: Saturated ground behaves like a liquid, causing buildings to sink.
  • Landslides: Triggered by ground movement on steep slopes.
  • Tsunamis: Caused by undersea earthquakes displacing water.
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4
Q

How do tsunamis form in 5 steps?

A
  • Underwater earthquakes cause seafloor displacement -> pushing water upwards -> Waves travel fast in deep water -> slow in shallow water -> increasing height.
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5
Q

What are the 3 impacts of tsunamis?

A
  • Widespread coastal flooding.
  • Infrastructure destruction (homes, roads, power lines).
  • Loss of life due to fast-moving waves.
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6
Q

When and where did the Gorkha earthquake occur?

A
  • 25 April 2015
  • Epicentre near Kathmandu, Nepal.
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7
Q

What were the 3 primary impacts of the Gorkha earthquake?

A
  • 9,000 deaths, 22,000 injuries.
  • 600,000 buildings destroyed.
  • Landslides and avalanches blocked roads and buried villages.
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8
Q

What were the 3 secondary impacts of the Gorkha earthquake?

A
  • Tourism decline (Everest climbing season cancelled).
  • Food and water shortages due to damaged infrastructure.
  • Aftershocks continued to cause damage.
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9
Q

What were the 3 immediate responses to the Gorkha earthquake?

A
  • Search and rescue operations by Nepalese army.
  • International aid sent (e.g., India and Indonesia provided relief supplies).
  • Tents and temporary shelters set up for displaced people.
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10
Q

What were the 3 long-term responses to the Gorkha earthquake?

A
  • Stricter building codes to make infrastructure earthquake-resistant.
  • Rebuilding efforts with international funding.
  • Improved disaster preparedness through early warning systems.
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11
Q

What are the 3 ways in which earthquakes be predicted?

A
  • Seismometers detect small tremors.
  • GPS monitoring tracks crustal movements.
  • Historical data helps identify high-risk areas.
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12
Q

What 3 strategies can reduce earthquake damage?

A
  • Earthquake-resistant buildings (shock absorbers, flexible materials).
  • Land-use zoning (keeping critical infrastructure away from fault zones).
  • Education and drills (teaching people what to do during an earthquake).
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13
Q

What is the focus?

A

where the pressure is released underground and where the energy radiates out from.

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14
Q

What is so special about the focus?

A

This is the place with the strongest waves that cause the most damage.

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15
Q

What is the epicenter?

A

the point directly above the centre of the earthquake on the earth’s surface.

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16
Q

What are seismic waves?

A

when energy is released from the focus in shock waves.

17
Q

What are the 3 types of earthquakes?

A

1) Shallow-focus
2) Deep-focus
3) Underwater

18
Q

What are shallow-focus earthquakes?

A

Earthquakes in which the focus is 0-70km under the Earth’s surface.

19
Q

What are deep-focus earthquakes?

A

when an earthquake has a focus which is 70-700km under the Earth’s surface.

20
Q

How are deep-focus earthquakes caused?

A

Deep-focus earthquakes are caused by previously subducted crust moving towards the core, heating up or decomposing.

21
Q

What do deep-focus earthquakes tend to be like?

A

They are generally less damaging than shallow-focus because the shock waves have to travel further and so cause less shaking at the surface.

22
Q

What is so special about underwater earthquakes?

A

They move the seabed, which causes water to get displaced. If enough water is displaced, tsunamis (series of enormous waves) can happen.

23
Q

Are underwater earthquakes deep or shallow focus?

A

They can be shallow- or deep-focus. The deeper the focus, the bigger the tsunami.

24
Q

What are the 3 types of waves?

A

1) P-waves
2) S-waves
3) L-waves

25
What are P-waves?
P-waves are the fastest waves but they cause the least damage.
26
What are S-waves?
Waves that make the ground shake violently.
27
What are L-waves and describe how they occur?
The waves that create significant damage, including crustal fracturing. They only travel across the surface and have a large amplitude.
28
Describe the process of liquefaction in 2 steps?
- Earthquakes compact loose sediment of silts, sand and gravel that are waterlogged. - The compact ground forces water to rise to the surface and damage to buildings and infrastructure is common.
29
What are the 5 characteristics of tsunamis?
1) Long wavelength at sea 2) short amplitude at sea 3) velocity 4) drawback 5) wave-train
30
What is wavelength?
the distance measured between two identical points of a wave.
31
Can you give a stat for long wavelength at sea in a tsunami?
The wavelength is often over 100km long
32
Can you give a stat for short amplitude at sea in a tsunami?
They are usually 1m in height and are barely noticeable but when they reach land, their height can increase to over 25m in some cases
33
Can you give a stat for velocity in a tsunami?
They move quickly in deep water and can reach speeds of up to 700 kph but they slow down as they reach shallow water
34
What is a drawback?
When there is a localized drop in sea level
35
What is a wave-train?
The way that a tsunami hits a coastline is like a series of waves
36
What was the magnitude of the gorkha earthquake
magnitude 7.8
37
Why does the geological structure of Nepal increases the risk of earthquakes? (Give 4 chains of reasoning)
- Pre-historic lakes filled many of the valleys so the sediment is soft ->The depth of soft sediment reaches 600 m deep in the Kathmandu valley -> So seismic waves that pass through this material are amplified -> causing structures to swing violently.