3.1.5.4 Seismic Hazards Flashcards

1
Q

What are seismic Hazards?

A

Plates do not move in fluid motions.

At any boundaries, plates become stuck due to the friction between plates.

The pressure builds so much that it cannot be sustained and the plates eventually give way.

The pressure is released quickly, causing a jolting motion in the plates.

This jolt is responsible for seismic movement spreading throughout the ground.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
2
Q

Focus Point

A

The focus is the point underground where the earthquake originates from.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
3
Q

Epicentre

A

The epicentre is the area above ground that is directly above the focus

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
4
Q

Secondary effects of seismic hazards

A
  • Shockwaves
  • Tsunamis
  • Liquefaction
  • Landslides
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
5
Q

Primary effect of Seismic Hazards

A
  • Earthquakes - ground shaking by the fracturing of rocks.
  • Sudden movements along fault lines.
  • Ground rupture
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
6
Q

Shockwaves

A

The shifting of rock in an earthquake causes energy to be released which vibrates through the ground creating shockwaves.

There are two types:

  • P-waves
  • S-waves (high amplitude, most destructive)
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
7
Q

Tsunamis

A

A tsunami is a giant sea wave generated by shallow-focus underwater earthquakes, volcanic eruptions and large landslides into the sea.

Tsunamis have a long wavelength and low wave height in the open ocean.

They travel at speeds of over 700kmh but when they reach shallow water, they increase in height.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
8
Q

Liquefaction

A

This is when violently shaken soils with a high water content lose their mechanical strength and become fluid.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
9
Q

Landslides

A

This is when there is slope failure as a result of the ground shaking.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
10
Q

Spatial distribution of earthquakes

A

The majority of earthquakes occur along plate boundaries, the most powerful at destructive margins and subduction zones.

There is a clear line of earthquakes along the centre of the Atlantic Ocean between the African and American Plates and around the Pacific Ocean at the edge of the Pacific plate.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
11
Q

Other places that earthquakes occur

A

Old fault lines: Some earthquakes occur away from plate boundaries and are associated with the reactivation of old fault lines.

Human activity: It has been suggested that human activity can lead to minor earthquakes, for example deep mine subsidence or fracking (fracturing of rock to release gas).

Hot spots: Isolated plumes of tectonic activity known as hot spots may give rise to seismic activity.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
12
Q

Earthquake magnitude measurement

A

The magnitude of an earthquake is measured by the:

  • Richter scale: logarithmic scale from 1-10 (7 is 10x than 6)
  • Moment magnitude scale (MMS): this identifies the energy release on a scale of 1-10
  • Mercalli scale: measures earthquake intensity through the impact on people and structures. The scale is 1-12.
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
13
Q

Frequency of earthquakes

A

Hundreds of low magnitude earthquakes happen around the world every day. (20000 a year)

The number of high magnitude earthquakes occur much less often. (An 8 or greater occur about once a year)

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
14
Q

Randomness vs regularity of earthquakes

A

Earthquakes don’t seem to follow any clear pattern or trend and their occurrence is random.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
15
Q

Predictability of seismic earthquakes

A

Scientists can monitor the movement of tectonic plates to predict which areas are at risk of seismic hazards.

However it is currently impossible to tell when an earthquake will strike a particular place and what magnitude it is likely to be.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
16
Q

Primary environmental impact

A
  • Earthquake can cause fault lines which destroy the environment
  • Liquefaction
17
Q

Secondary environmental impact

A
  • Radioactive materials and other dangerous substances leaked from power plants
  • Saltwater from tsunamis flood freshwater ecosystems
  • Soil salinization
18
Q

Primary economic impact

A
  • Businesses destroyed
19
Q

Secondary economic impact

A
  • Economic decline as businesses are destroyed (tax breaks etc.)
  • High cost of rebuilding and insurance pay out
  • Sources of income lost
20
Q

Primary social impact

A
  • Buildings collapse, killing / injuring people and trapping them
21
Q

Secondary social impact

A
  • Gas pipes rupture, starting fires which can kill
  • Water supplies are contaminated as pipes burst, spreading disease and causing floods
  • Tsunamis which lead to damaging flooding
22
Q

Primary political impacts

A
  • Government buildings destroyed
23
Q

Secondary political impacts

A
  • Political unrest from food shortages or water shortages
  • Borrowing money for international aid
  • Can be initial chaos and ‘lawlessness’ e.g. looting
24
Q

Short term responses

A
  • Evacuation
  • Providing health care
  • Providing emergency food and water supplies
  • Providing emergency shelter
25
Q

Long term responses

A
  • Prevention
  • Preparedness
  • Mitigation
  • Adaption
26
Q

Prevention of seismic hazards

A

Earthquakes and tsunamis will occur regardless so cannot be prevented.

However liquefaction can be prevented through soil stabilization (gravel columns in the ground), and avalanches can be prevented through controlled explosions.

27
Q

Preparedness for seismic hazards

A

Earthquake prone areas have extensive awareness strategies and education in place.

Earthquake warning systems and tsunami warning systems can be put in place.

Evacuation plans and training can also be put in place.

28
Q

Prediction of seismic hazards

A

Prediction can be very difficult however regions at risk can be identified.

Attempts to predict include:

  • Monitoring ground water levels
  • Monitoring release of radon gas
  • Strange animal behaviour
  • Measuring magnetic fields
29
Q

Mitigation of seismic hazards

A

Demolishing older unsafe buildings.

Tsunami wave breaks and sea walls.

30
Q

Adaption from seismic hazards

A

Move away from areas at risk.

Capitalise on opportunities such as encouraging tourism.

Insurance if living in places of risk.

Building specially designed earthquake proof buildings.