Seismic Hazards Flashcards

1
Q

seismic hazards (5)

A

primary
shockwaves

secondary
tsunamis
landslides
liquefaction

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2
Q

Types of seismic waves

A

Body waves
Primary (P waves)
- fastest
- solid and liquid
- least damaging

Secondary (S waves)
- slower
- solids only
- more damaging

Surface waves
Love (L waves)
- slowest
- side to side motion
- more destructive

Reylaigh

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3
Q

tsunamis

A

triggered by underwater earthquakes
- moves seabed which displaces large volumes of water
- creates large waves

travel very fast
little warning

eg 2004 indian ocean

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4
Q

Tsunami example

A

2004 Indian Ocean Tsunami
Final death toll - 283,000
Across many countries
1.7 million displaced

Spread of disease, contaminated water
Flooding - salinisation, loss of agriculture

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5
Q

landslides / avalanche

A

shaking of ground can dislodge rocks, soil or snow
moves downslope quickly

shaking also loosens material
easier for water to infiltrate
weight of more water trigger landslide after event

eg Nepal - over 3000

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6
Q

liquefaction

A

happens on saturated, uncompacted soil

vibrations cause it to act like a liquid
soil weaker (loses strength) and easier to deform

more likely to subside, especially under weight of buildings

Causes building and infrastructure collapse

eg Christchurch - 20,000 properties

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7
Q

distribution

A

95% at plate boundaries

can help with prediction - know areas at risk

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8
Q

magnitude

A

measured on rictor scale

destructive margins - higher magnitude
subduction zone causes massive pressure

deep focus - higher magnitude
but less damage as further from surface

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9
Q

frequency

A

high magnitude happen less frequently
- need time for pressure to build up

many small magnitude ones happen very frequently

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10
Q

randomness/ regularity

A

not clear pattern
unpredictable

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11
Q

predictability

A

impossible to predict
- hard to evacuate and prepare

seismic gap help predict magnitude (longer gap = higher)
know areas at risk
can monitor local tectonic activity

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12
Q

primary impacts

A

social
- building collapse, homelessness and death

economic
- destroy business

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13
Q

secondary impacts

A

social
- lack of water, gas and power, damage
- spread of disease, often in shelters
- landslides

env
- tsunamis

political
- conflict and political unrest - lack of supplies

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14
Q

short term responses

A

search and rescue
aid

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15
Q

long term responses

A

reconstruction - life safe
review emergency plans
tsunami warnings
education

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16
Q

preparedness

A

warning systems
- detect small seismic activity, may be indicator of larger one
- but very short notice

evacuation plans
education in schools

tsunami wanring systems

search and rescue

17
Q

mitigation

A

emergency plans in place

search and rescue prepared

life safe buildings

18
Q

prevention

A

not possible

prevent risk
- not build on land pine to liquefaction
- sea walls for tsunamis

19
Q

adaptation

A

life safe buildings
- designed to withstand shaking

also less vulnerable to tsunamis
- tall and strong

20
Q

Are tsunamis or earthquakes on land worse?

A

2004 Indian Ocean Tsnumai
283,000 deaths
Disease and loss of agriculture

Nepal
9000 death

Tsunamis worse
But less frequent than land earthquakes, narrow coastal belts they can effect

21
Q

Conservative

A

Shallow (no subduction)
Narrow zone
Low frequency (friction, pressure builds up)
Hugh magnitude

22
Q

Constructive

A

Shallow
Narrow
Regular
Low magnitude (as more frequent)

23
Q

Destructive subduction

A

Deep
Wide
Infrequent
High magnitude

24
Q

Destructive collision

A

Shallow (no subduction)