Hazards Flashcards

1
Q

What are body waves? List 2 types of body wave too.

A

Waves that travel through the earth. They are either the primary or secondary type.

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2
Q

How do primary/pressure waves work?

A

Like a slinky, they alternatively compress and expand. Particle motion is parallel to wave movement here. They can travel through ALL substances, and are the fastest type of wave.

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3
Q

In context with some land, explain how primary waves would impact this?

A

Primary waves cause rocks to move back and forth making the ground break up.

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4
Q

How do secondary (AKA sheer or shaking) waves work?

A

A transverse movement of particles that is 90 degrees (perpendicular) from the movement of the wave. However it cannot travel through air or water, they are slower but cause more damage than primary waves. It’s like shaking a rope, or the sound waves you get which are transverse (oscillating in right angles to wave movement).

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5
Q

In context with some land, explain how secondary waves would impact this?

A

Secondary waves cause the ground to shake up and down.

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6
Q

What are surface waves? List 2 types of these waves too.

A

Travel along the earth’s surface, cause the most damage, as they cause more ground movement and travel more slowly so take longer to pass. 2 Types of surface waves are the Raleigh and love wave.

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7
Q

How do Raleigh waves work?

A

Rock moves in an elliptical motion to as the wave moves horizontally and this clock-like movement breaks up the ground. It’s like a ground roll. Similar to surface water waves.

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8
Q

How do love waves work?

A

Horizontal sheer waves, move the ground from side to side at right angles to the direction of the movement. This damages infrastructure and buildings.

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9
Q

List primary effects of seismic events [2]

A

Ground ruptures and ground shaking.

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10
Q

What is the level of ground shaking (primary effect of seismic activity) dependent on?

A

Magnitude, depth of focus, distance from epicenter and local geological conditions

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11
Q

What’s a ground rupture?

A

Displacement of the earth’s surface along a fault line

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12
Q

Give an example of a secondary effect of a seismic event that occurs in the hydrosphere?

A

Tsunamis

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13
Q

How does a tsunami form due to seismic activity

A

Formation:
Earthquake vertically moves the seabed up by several meters. Displacing (moving) the water above.
Large waves radiate outwards across the ocean away from the epicentre of the earthquake.
When it reaches shallow water near the coast, the base is slowed down by friction and becomes taller. This is called shoaling.
A large wave hits the coast, a tsunami.

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14
Q

Factors that affect tsunami strength? List [4]

A
  • Distance wave has travelled.
  • Coastal geography: relief of the coastline.
  • Coastal land use and population density.
  • Lack of warning systems and evacuation plans.
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15
Q

Why does the distance the wave has travelled affect tsunami strength?

A

This is because as waves travel, they lose energy - this means that the further away from the coast an earthquake occurs, the less powerful it is when it reaches the coast.

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16
Q

Hazards can be classified as a mixture of these geographic processes (geophysical, hydrological and atmospheric). Give an example

A

A tropical storm. Hydrological / Atmospheric, as both of these processes contribute to the hazard. The heavy rainfall is a result of atmospheric and hydrological interactions, and interaction of low and high pressure is atmospheric.

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17
Q

Give 4 factors that can affect hazard perception

A
  • Wealth
  • Past experiences
  • Education
  • Religion
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18
Q

How can wealth affect hazard perception?

A

Wealthier people may percieve a hazard to be smaller, as they are less vulnerable. As a result, they may not partake in preparation and evacuation - heightening their risk.

However, wealthier people may view hazards as a greater risk, due to heightened costs of property damage and financial loss than someone less wealthy. This is dependent on the person.

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19
Q

How can experience affect hazard perception?

A

Someone who’s experienced more hazards may be more likely to understand the full effects of a hazard.

Studies also suggest that people who have experienced
hazards are likely to have an optimistic and unrealistic outlook on future hazards, almost like a
‘lightning never strikes twice”.

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20
Q

How can education affect hazard perception?

A

A person who is more educated about hazards may understand their full effects on
people and how devastating they can be and have been in the past.

Those who are less educated
may not understand the full extent of a hazard and may not evacuate etc.

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21
Q

How can religion affect hazard perception?

A

Some may view hazards as put there by God for a reason, or being part of the natural cycle of life. So may not percieve them to be negative.

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22
Q

How can mobility (highly reliant on age) affect hazard perception?

A

Those who have limited access to escape a hazard may perceive hazards to be
greater threats than they are.

Whether they are in a secluded location, or if they are impaired with
a disability or illness, those who cannot easily leave an area quickly may feel more at risk, so may take extra effort to evacuate quickly

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23
Q

What’s a passive response to a hazard?

A

fatalist attitude - doing nothing, and letting the hazard impact you.

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24
Q

What viewpoint does fatalism adopt?

A

hazards are uncontrollable natural events. Any losses should be accepted as nothing can be done to stop them.

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25
Q

Give examples of active responses to a hazard. There are 5.

A

Prediction, Adaption, Mitigation, Management, Risk Sharing

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26
Q

What viewpoint does Prediction adopt? Also what does it sometimes manage to do to natural hazards?

A

Using scientific research and past events to know when a hazard will take place, therefore warnings can be delivered > impacts reduced.

In some cases, prediction helps stop hazards altogether before they start. (i.e. wildfires as a result of a long drought).

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27
Q

What viewpoint does adaption adopt?

A

Attempting to live with hazards by adjusting lifestyles and settings of people, so that vulnerability to the hazard is lessened (i.e. earthquake proof houses).

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28
Q

What viewpoint does mitigation adopt?

A

Strategies carried out to lessen hazard severity. sandbags to offset flood impacts

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29
Q

What viewpoint does management adopt?

A

Coordinated strategies to reduce a hazard’s effects. Including prediction, adaption, mitigation.

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30
Q

What viewpoint does risk sharing adopt? And what does it consist of as a process?

A

A form of community prepardness,

where the risk posed by a natural hazard is shared by the community, they all invest collectively to lessen (mitigate) the impacts of future hazards.

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31
Q

What’s the case study for risk sharing?

A

New Zealand

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32
Q

What types of hazards do New Zealand have?

A

earthquakes, volcanoes, tsunamis, weather related hazards - making it a multi hazard environment.

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33
Q

How is New Zealand affected by these multiple hazards?

A

Mainly cost wise. The Cantebury Earthquake in 2010 cost the country 20% of all national GDP.

34
Q

How are New Zealand attempting to reduce risk after 2010 Canterbury Earthquake?

A

strategies are put into place before disasters, rather than investing more to clean it up.

35
Q

How can hazards vary? List 3 factors?

A

Location, frequency and strength

36
Q

What is incidence of a hazard, and explain why low incidence hazards are so hard to predict & intense?

A
  • How often a hazard occurs.
  • Low incidence hazard > harder to predict and have less management strategies put in place > hazard could be more catastrophic when it occurs.

Also, these Low incidence hazards are usually more intense that high.

37
Q

Give some statistics to show why low incidence hazards are higher magnitude than high incidence?

A
  • only 36 recorded earthquakes since 1500 have had magnitude 8.5 or higher, but millions that are too weak to be recorded are thought to happen every year.
38
Q

What’s distribution in terms of a hazard?

A

where hazards occur geographically

39
Q

How can distribution affect hazard intensity?

A

Areas of high hazard distribution are likely to have a lot of management strategies > adapted to hazardous landscape.

40
Q

What’s intensity in terms of a hazard?

A

The power of the hazard. How strong it is and how damaging its effects are.

41
Q

What’s magnitude in terms of a hazard?

A

size of the hazard, usually this is how intensity of a hazard is measured.

42
Q

What happens if hazards are high intensity (magnitude), what does this mean for management?

A

Worse effects > require more management > more mitigation strategies will be needed to lessen the effects and ensure a relatively normal life can be carried out post-hazard.

43
Q

How does level of development affect how a place can respond to a hazard?

A

A hazard with the same magnitude may have very different efects in two places contrasting in development levels > hazards in LICs > less likely to have effective mitigation strategies due to cost > effects of hazard are much more likely to be catastrophic here.

44
Q

Which HIC was not prepared for hazards?

A

Multi hazard environments such as New Zealand

45
Q

Why may HICs not be prepared for hazards?

A

lack of management strategies > (true mostly in multi hazard environments) > resources spread thinly over different hazards > less focused on 1 particular hazard

46
Q

Give an example of an HIC not prepared for hazards and what hazard

A

Canada, wildfires

47
Q

What is a hazard in simple terms

A

a potential threat to human life and property caused by a natural/manmade event.

48
Q

What are the 3 types of major hazards

A

Geophysical, atmospheric & hydrological

49
Q

What’s a geophysical hazard - give an example too

A

A hazard driven by the earth’s internal processes (internal process example - the interaction of 2 plate boundaries, causing volcanoes). This can be a volcano, or seismic activity.

50
Q

What hazards impact the Phillipines

A

Volanic eruptions, seismic events, typhoons, flooding, landslides

51
Q

Why do volcanoes occur in Phillipines ?

A

Because it’s on a destructive plate boundary, Philippine plate subducted. Therefore, events will be less frequent and high magnitude. Therefore, pyroclastic flows also occur do to the pressure buildup from viscous lava.

Pinatubo caused worldwide effects

52
Q

Why do seismic events occur in Phillipines?

A

Near a destructive plate > high magnitude seismic events such as Bohol Magnitude 7.2 which killed 200.

53
Q

Why do Typhoons occur in Phillipines

A

Phillipines within 5-20N of the equator (also affected by ITCZ solar insolation)> vunerable due to warm ocean waters of the west Pacific > 710 typhoons annually.

54
Q

Secondary hazards of Philliplnes

A

Landslides: due to heavy rainfall from typhoons and due to unstable land from tectonics.

55
Q

How do hazards impact on the Phillipines?

A

Affect economic development: as money must go into damage recovery and improving future responses.

Hazards caused £26bn from 500 events since 1990.

56
Q

Why are people in the Phillipines so vulnerable?

A

Due to coastally distributed population.

Landslide distaster risk has increased as the pressures of an increasing population lead to deforestation of upland areas. (due to less tightly held together soil, and more surface runoff).

Widespread poverty.

57
Q

Why is the Phillipines so at risk of hazards as a nation?

A
  • LIC, therefore less able to cope with the financial impacts of natural disasters (unable to mitigate risk for next time the event occurs).
  • Near a destructive plate boundary - can prompt natural hazards such as earthquakes and volcanoes. (multi-hazardous therefore).
  • Between latitudes 5-20 degrees, therefore at risk of monsoon rainfall, which can have secondary impacts such as landslides. These require lots of money to repair the lives of those affected, the LIC country may not have.
  • Hundreds of Islands (populations spread out), therefore evacuation in the Response stage of the hazard management cycle is made trickier - more vehicles required for evacuation & also harder communication between islands.
  • High population density in Manilla (capital of PH - a megacity) > as so many are living together, a greater impact socially and finacially is possible. (up to 2,000 per km2)
58
Q

Why are natural hazards made so hazardous to humans?

A

They live in disaster zones (if a volcanic event occured where no one lived, it wouldn’t be a natural hazard).

59
Q

What is risk?

A

The exposure of people to hazards.

60
Q

Why do people put themselves at risk?

A

Unpredictable: not very frequent, thinks it won’t happen to them.
Lack of alternatives: if they’re poor (poverty) no choice to live?
Cost/Benefit: some live in fertile areas (agri industry), or have job benefits.
Changing risk levels: deforestation - people move when low risk, then it becomes high risk over time. Not aware of this risk?

61
Q

What’s vulnerability?

A

Potential for loss. of life of possessions.(Mainly focussed on wealth).

62
Q

A country gets more money, how does its risk and vulnerability change?

A

Risk remains the same, still affected by the same natural hazards.

Vulnerability: Less vulnerable, as more able to afford better protection.

63
Q

What are the different scales of risk mitigation (reducing risk)

A

Government and individual:

I - ex. choosing to locate on higher ground in a flood prone region.

G - ex. emergency plans for evacuation in place for a hazard.

64
Q

How does community resilience work?

A

Communities utilise resources available (through gov funds) , able to withstand and recover - minimising the hazard’s effect, making it easier to return to a normal life. A collective investment of communities.

65
Q

How does Integrated Risk Management Work?

A

Identify: see where you live, is it near a hazard?
Analyse: the extent of the risk
Priorities: look at those more vulnerable? (i.e. Poorer people)
Plan: plan strategy (investment, and responses)
Public awareness: educating the public on the risk.
Communication: at time of hazard, warnings are provided for evacuation awareness.
Monitor: used for prediction, can allow faster responses.

66
Q

3 P’s risk management? How does it work?

A

Prediction: predict and provide warnings after (i.e. satellite images, sensors in seas help predict earthquakes, can prevent impacts of tsunamis as secondary impacts.

Prevent: can reduce extent of natural hazard - storms: seed clouds - create more clouds in storm area, this weakens storm.

Protection: protect people’s possessions and environment: builds made quake proof/flood defences.

67
Q

What does Park’s curve demonstrate?

A

How hazards have varying effects over time & comparative accross many events.

68
Q

What’s distribtion in terms of a hazard?

A

Spatial coverage of a hazard. Local or global: storm can be local, global can be underwater quake causing secondary effect tsunami leading to flooding.

69
Q

What’s frequency in terms of a hazard?

A

Distribution of hazards through time:

case study: ring of fire - area of plate boundaries, where volcanoes and quakes take place frequently. Frequency higher along ring of fire, less frequent intraplate.

70
Q

What was the volcano in 1991, Phillipines

A

MT pinatubo

71
Q

Where did MT Pinatubo occur in the Phillipines, and how many years was 1991 since its last eruption?

A

After 500 years lying dormant in June 1991 Mount Pinatubo erupted on the island of Luzon, it being the
second biggest in the 20th century.

72
Q

How did MT Pinatube form?

A

The subduction of the Eurasian plate beneath the Phillipines plate at a destructive plate boundary in West of Luzon.

73
Q

What happened straight after eruption? (Global impact too)

A

A large amount of ash released into the atmosphere caused pyroclastic flows and lahars.

Global temperatures were lowered 0.5C, due to the combo of ash and sulphur dioxide in the atmosphere, for 2 years following the eruption.

74
Q

List 3 social impacts of the eruption Pinatubo, 1991, Phillipines

A

Secondary impact: 100 killed by lahar mud flows.

Response: 58,000 evacuated within a 30km radius of the volcano.

Poverty: 1.2 million people lost their homes
who lived at the volcanoes base. They were forced to live in shanty towns in
Manila, where sanitation is poor and
housing is dangerous.

75
Q

List 3 economic impacts of the eruption Pinatubo, 1991, Phillipines

A

LFinancial losses: est. $700m of damages to homes/infrastructure.

Agri Impacts: heavy rain and ash meant that land turned unusable , 650,000 farmers lost their jobs. Many in PH rely on farming as a main source of income.

Global connections: the airport had to be closed stopping tourism for sometime and the export of goods.

76
Q

List 3 environmental impacts of the eruption Pinatubo, 1991, Phillipines

A

River destruction: Fast flowing lahars causes severe river bank erosion and undercut bridges.

Farmland: Agri land became unusable.

Global Impact: The combination of the ash and the sulphur dioxide in the atmosphere lowered global temperatures by 0.5C between 1991 and 1993.

77
Q

When was the Guinsaugon mudslide, and how deep was it. Also, how many cubic metres covered the village? (Phillipoines)

A

17th February 2006.

Mudslide covered 9 km2, was 3km wide and had a maximum depth of 30 meters.

Around 1.2 billion cubic meters of mud covered the village.

78
Q

Why did the Guinsaugon mudslide in Phillipines occur

A

heavy rainfall due to the La Nina event in the western pacific.

In 10 days, 200cm of rain had fell which severely saturated the already unstable slopes. (unstable due to earthquakes).

79
Q

How did the previous 2.6 mag (small) earthquake before the Guinsaugon Phillipines mudslide impact it?

A

Caused unstable ground (liquefaction)

80
Q

How did human factors mean that the Guinsaugon Phillipines mudslide occured.

A

deforestation that has occurred over the past 70 years, due to population
growth increasing the demand for food, as well as illegal logging in the region.

Therefore less interception (more saturated soils) and also less roots to stabilise soils.

81
Q

List 3 impacts of Guinsaugon Phillipines Mudslide:

A

SPEED: <1,000 people killed incl. 246 children at school. due to speed at
which the event occurred. No one could escape with one villager describing it as a “wall of mud”

HOUSES GONE: Virtually all of the 300 houses that once stood in the village had been destroyed.

FARMING KILLED: Valuable faming land used for agriculture was buried under many meters of mud, whilst livestock were killed.

82
Q

What made Typhoon Hayaan in Phillipines special? How large were wind speeds, and what category typhoon was it?

A

The Philippines was hit by one of the strongest typhoons ever recorded. It was a Category 4 or 5 typhoon and had sustained wind speeds up 150mph.