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Aa Hodder Geography > Hazards > Flashcards

Flashcards in Hazards Deck (473):
1

What is a natural hazard

A perceived event that threatens both life and property. They occur in the physical environments of the atmosphere, lithosphere and the hydrosphere

2

What do natural hazards result in

Disasters that cause some loss of life and/or damage to the built environment and create severe disruption to human activities

3

What do natural/environmental hazards include

Volcanic activity, seismic events and tropical storms

4

What are some examples of disruption to human systems

Death and injury, property and communication system damage and the disruption of economic activities

5

How is the risk of hazards posing a risk to human population increased

Because of built shanty towns on unstable tropical slopes, urbanisation of volcanic zones, people live in areas with active faults and also in coasts susceptible to hurricanes and tsunamis. The risk is also exacerbated by the failure to recognise a potential hazard and react accordingly

6

What are the 5 common characteristics of natural hazards and their effects on people

Origins are clear and effects they produce are distinctive.
Most only allow a short warning time before they hit.
Exposure to the risk is usually involuntary.
Most losses to life and damage to property occur shortly after the event.
The scale and intensity of the event requires an emergency response.

7

Where does the characteristic of the exposure to risk being involuntary apply to usually

To the populations of less well developed countries, people in developed areas who choose to live in hazardous zones are often well aware of the risks which they choose to minimise or even ignore

8

Examples of the effects of natural disasters being felt in communities a long time after the event has occurred

Disease, disruption to communities and economic activity

9

What is adaption in the context of hazards

The attempts by people or communities to live with hazard events. By readjusting their living conditions, people are able to reduce their levels of vulnerability.

10

Examples of adaption in the context of hazards

They may avoid building on sites that are vulnerable to storm surges but stay within the same area

11

What is fatalism

A view of a hazard event that suggests that people cannot influence or shape the outcome, therefore nothing can be done to mitigate against it. In some parts of the world, the outcome of a hazard event can be said to be ‘God’s will’

12

What do people who believe in fatalism do to mitigate the risks of a hazard

They put in place limited or no preventive measures

13

What is perception

This is the way an individual or a group views the threat of a hazard event. This will ultimately determine the course of action taken by individuals or the response they expect from governments and other organisations

14

What is risk

The exposure of people to a hazardous event presenting a potential threat to themselves, their passions and the built environment in which they live

15

What are 5 reasons people consciously put themselves at risk from natural hazards

Hazard events are unpredictable.
There’s a lack of alternatives.
Changing levels of risk.
Cost/benefit analysis.
Perception.

16

How is hazard events being unpredictable a reason for people choosing to live in hazardous areas

One can not predict the frequency, magnitude or scale of a natural hazard event

17

How is the lack of alternatives a reason for people choosing to live in hazardous areas

Due to social, political, economic and cultural factors, people cannot simply uproot themselves from one place and move to another, giving up their homes, land and employment

18

How is the changing level of risk a reason for people choosing to live in hazardous areas

Places that were once relatively safe may have become through time far more of a risk.

19

Example of changing levels of risk causing people to live in risky areas that once weren’t risky

Deforestation could result in more flooding from torrential rain associated with tropical storms and there could also be a greater risk from landslides

20

How is the cost/benefit analysis a reason for people choosing to live in hazardous areas

There are many hazardous areas that offer advantages that in people’s mind outweigh the risk that they are taking.

21

Example of the cost/benefit analysis causing people to live in risky areas

Californian cities for example have a high risk from earthquakes, but people see the many advantages of living there as greater than the potential risk

22

What does vulnerability to physical hazards mean

The potential for loss

23

Why does vulnerability vary over time and space

Since loses vary geographically, over time and among different social groups

24

Who came up with the model of vulnerability

Researchers at the University of South Carolina

25

What does the model of vulnerability look like

Risk and mitigation creates the hazard potential.
Hazard potential to geographic context and social fabric.
Geographic context to biophysical vulnerability.
Social fabric to social vulnerability.
Biophysical vulnerability and social vulnerability to place vulnerability.
Place vulnerability back to risk and mitigation.

26

What are some examples geographic context in the model of vulnerability

Physical setting
Proximity

27

What are some examples social fabric in the model of vulnerability

Experience
Perception
Built environment

28

What can effect the degree to which the hazard event will impact upon them

People wealth and the level of technology that they can apply

29

How can richer people and counties protect themselves from hazard

By building sea defences, constructing earth-quake resident buildings, providing better emergency services etc.
They can be better prepared by being made more aware of their risk through education

30

Why have more and more people been forced to live in hazardous areas

As urban areas have grown so has the population

31

What are low lying areas of cities at risk form

Tropical storms and tsunamis

32

Why do people react to the threat of hazards in different ways

Because of the way in which individuals receive and process information

33

What 7 factors effect perception

Socio-economic status
Level of education
Occupation/employment status
Religion, cultural/ethnic background
Family and marital status
Past experience
Values, personality and expectations

34

What do perceptions of hazards ultimately determine

The course of action taken by individuals in order to modify the event or the responses they expect from governments and other organisations

35

When is there often a greater difference in the perception of a hazard

Between people of differing levels of economic development

36

What is the idea that ‘in wealthier areas there is a sense that the better that you are prepared, the more you will be able to withstand the impact of a hazard’ based upon

Government and community action and is usually backed by capital that will fund technologically-based solutions

37

When does the sense of helplessness in the face of a natural hazard tend to increase

With the level of poverty and the deprivation of the people

38

What do disadvantaged people in wealthy counties usually see natural hazards as

Part of their way of life, unavoidable much like the bulk of people in poorer countries seeing the impacts of these events as being part of the conditions of overtly

39

What 3 ways may people perceive natural hazards

Fatalism (acceptance)
Adaption
Fear

40

How is the ‘adaption’ perception of a natural hazard carried out

People see that they can prepare for, and therefore survive the events by prediction, prevention and/or protection, depending upon the economic and technological circumstances of the area in question

41

How is the ‘fear’ perception of a natural hazard carried out

The perception of the hazard is such that people feel so vulnerable to an event that they are no longer able to face living in the area and move away to regions perceived to be unaffected by the hazard

42

What does community preparedness/risk sharing involve

Prearranged measures that aim to reduce the loss of life and property damage through public education and awareness programmes, evacuation procedures, the provision of emergency medical, food and shelter supplies and the taking out of insurance

43

What does frequency mean

The distribution of a hazard through time

44

What is the process of integrated risk management

Considering the social, economic and political factors involved in risk analysis; determining the acceptability of damage/disruption; deciding on the actions to be taken to minimise damage/disruption

45

What is magnitude

The assessment of the size of the impact of a hazard event

46

What is prediction

The ability to give warnings so that actions can be taken to reduce the impact of hazard events. Improved monitoring, information and communications technology have meant that predicting hazards and issuing warnings have become important in recent years

47

What are primary effects

The effects of a hazard event that result directly from that event. For a volcanic eruption these could include lava and pyroclastic flows. In an earthquake, ground shaking and rupturing are primary effects

48

What is community resilience

The sustained ability of individuals or communities to be able to utilise available resources to respond to, withstand and recover from the effects of natural hazard events. Communities that are resilient are able to minimise the effects of the event, enabling them to return to normal life as soon as possible

49

What are secondary effects

The effects that result from the primary impacts of the hazard event. In volcanic eruptions these include flooding (from melting ice caps and glaciers) and Lahars. In an earthquake, tsunamis and fires (from ruptured gas pipes) are secondary effects

50

Where can responses to natural hazards come from

Individuals, the local community with people working together, and from national governments and international agencies

51

What is a key feature of the modern approach to managing hazards

That hazards are best combated by efficient management

52

What do modern management techniques of natural hazards aim to do

Using their gathered information, careful analysis and deliberate planning, they aim to make the most efficient use of the money available to confront natural hazards

53

Example of a modern approach to managing natural hazards

Integrated risk management

54

What are the incorporated parts of the integrated risk management

Identification of the hazard.
Analysis of the risks.
Establishing priorities.
Treating the risk and implementing a risk reduction plan.
Developing public awareness and a community strategy.
Monitoring and reviewing the whole process.

55

What 3 ways do people and organisations try to manage natural hazards

Prediction
Prevention
Protection.

56

What is the key to predicting hazards in managing them

Improved monitoring in order to predictions which means the warnings can be issued

57

Example of agency that uses prediction depends upon monitoring information from satellites and recordings of land, sea and air

The National Hurricane Centre in Florida

58

For natural hazards, why is prevention unrealistic

Because it is too difficult to stop a natural disaster from occurring

59

Examples of prevention of natural hazards

Seeding clouds in potential tropical storms in order to cause more precipitation, which in theory would result in a weakening of the system as it approaches land

60

What is the aim of protection in managing natural hazards

To protect people, their possessions and the built environment from the impact of the event

61

What does protection in managing a natural hazard usually involve

Modifications to the built environment such as improved sea walls and earthquake proof buildings

62

What is one way in which governments can act, and people react, to help manage natural hazards

To try and change attitudes and behaviour to natural hazards which will reduce people’s vulnerability. Community preparedness.

63

What must all attempts at managing natural hazards be evaluated in terms of

Their success

64

Example of successful schemes in managing natural hazards

Dynamite to divert lava flows on Mt Etna and pouring sea water on lava flows in Iceland

65

Example of an unsuccessful scheme in managing natural hazards

The Japanese felt they were well prepared for earthquakes and yet in 1995 the city of Kobe suffered the Great Hanshin earthquake, which destroyed over 100,000 buildings, a death toll over 6,000 and 35,000 injuries

66

What can be used to evaluate schemes to manage natural hazards

The disaster/risk management cycle

67

What does the disaster/risk management cycle illustrate

The ongoing process by which governments, businesses and society plan for and reduce the impact of disasters, react during and immediately following an event, and take steps to recover after an event has occurred

68

What do appropriate actions at all points in the disaster/risk management cycle lead to

Greater preparedness, better warnings and reduced vulnerability or the prevent of hazard events during the next cycle

69

What does the complete disaster/risk management cycle include

The shaking of public policies and plans that either modify the causes of the hazard events or mitigate their effects on people, property and infrastructure

70

What are the three parts to the disaster/risk management cycle

Pre-disaster: risk assessment, mitigation/preventing, preparedness
Response: warning/evacuation, saving people, providing immediate assistance, assessing damaging, ongoing assistance
Post-disaster: restoration of infrastructure, reconstruction, economic and social recovery, ongoing development activities, risk assessment, mitigation/ prevention

71

What is one of the main goals of disaster management (and one of its strongest links with development)

The promotion of sustainable livelihoods and their protection and recovery during such events

72

Where the goal of disaster management of ‘promotion of sustainable livelihoods and their protection and recovery during such events’ is achieved what happens

People have a greater capacity to deal with with disasters and their recovery is more rapid and long lasting

73

What is the Federal Emergency Management Agency (FEMA) main purpose

To co-ordinate the response to a disaster that has occurred in the United States and that has overwhelmed the resources of local and state authorities

74

What have FEMA created

Major analysis programmes for floods, hurricanes and earthquakes

75

Where are the operations by FEMA ferried our

Along the lines shown by the disaster/risk management cycle

76

What are the different ways of managing natural hazards

Community resilience
Integrated risk management
Prediction, prevention, protection
Community preparedness

77

What are the two ways attempts at managing hazards can be assessed

Disaster/risk cycle
Disaster/response curve

78

Who devised the disaster/response curve

Park

79

Why did Park devise the disaster/response curve

To show that hazard events can have varying impacts over time

80

What does the disaster/response curve show

An early stage, before the disaster strikes, where the quality of life is normal for the area. Here people try their best to prevent such events and prepare in case they should happen. When the event happens, the quality of life suddenly drops with people taking immediate action to preserve life and, if possible the built environment to bring the quality of life back to normality

81

What are the components in Parks disaster/response curve

Along the y axis: quality of life. Level of economic activity. Social stability communications/service level.
Along the x axis: time.
In the graph: the top is improvement in yellow, second section is normality and third section is deterioration.
The hazard event is the red line that usually starts in normality and drops due to disruption. The line then increases with recovery.

Pre-disaster: relief, rehabilitation, reconstruction. All along the x-axis

82

What is the stage in Parks model called relief

Starts as soon as the disaster strikes.
Relief is where medical attention, rescue services and overall care are delivered. This can last form a few hours to several days if the event has been damaging. From this point the quality of life of the people of the area starts to slowly increase.

83

What is the stage in Parks model called rehabilitation

Quality of life is still in the deterioration zone but it is rising.
Where people try to return the state or things to normal by providing food, water and shelter for those most affected. This period can last anything from a few days to weeks

84

What is the stage in Parks model called reconstruction

Quality of life is rising rapidly and is going back to the normality zone.
Where the infrastructure and property are reconstructed and crops regrown. At this time people use the experience of the event to try to learn how to better respond to the next one. This period can take from weeks to several years.

85

How can their be variations within the Park model

The model will be different due to different speeds of the drop in the quality of life, the duration of the decline and the speed and nature of recovery - e.g some places may never recover to their normal quality of life or some may recover to a better one.

86

What could variations within the park model be due to

It could be related to the type of hazard, the degree of preparedness or the speed of the relief effort and the nature of recovery and rebuilding

87

What is distribution

The spatial coverage of the hazard, this can refer to the area affected by a single event, which can have a localised effect, while others have a wider effect like tsunamis which can cross large oceans.
It can also refer to the areas where he particular hazard is likely to occur.

88

What have volcanic eruptions been known to have

A global effect with the spread of dust and the consequent short-term climatic change

89

What is the usual distribution of earthquakes and volcanoes

Generally they are associated with tectonic plate boundaries

90

What is the usual distribution of tropical cyclones

Usually between 5* and 25* north and south of the equator

91

At its most basic level, what does the frequency-magnitude principle lead us to expect

Many small insignificant events and, in the long term, increasingly fewer events as magnitudes rise

92

What would be the primary effects for an earthquake

Ground shaking and cracking

93

What would be the secondary impacts of an earthquake

Soil liquification, landslides, tsunamis and the effects on people and the built environment such as collapsing buildings, fires, flooding and the knock on effects which could be with the population for a long time

94

How may the legacy of a hazard event be around for years

Communication systems could be out of order.
The ability to produce food crops may take some time to be restored.
The economy of a region may be severely damaged for years.

95

Before the development of plate tectonic theory, what did the Earth scientists divide the interior of the earth into

3 layers: the crust, the mantle and the core

96

What is the core made up of

Dense rocks containing iron and nickel alloys

97

What is the core divided up into

A solid inner core and a molten outer one, with a temperate over 5000*C

98

How is the heat in the earths core produced

Mainly as a result of two processes: primordial heat and radiogenic heat

99

What is primordial heat

Heat left over from the earths formation

100

What is radiogenic heat

Produced by the radioactive decay of isotopes, particular uranium-238, thorium-232, potassium-40

101

What is the mantle made up of

Molten and semi-molten rocks containing lighter elements such as silicon and oxygen

102

Why is the crust light

Because of the elements that are present, the most abundant being silicon, oxygen, aluminium, potassium and sodium

103

How does the crust vary in thickness

Beneath the ocean it is only 6-10km thick but below the continents this increases to 30-40km and under the highest mountain ranges this can be as high as 70km

104

What has the theory of plate tectonics retained

The division of the 3 layers but new research suggests the crust and upper mantle should be divided into the lithosphere and asthenosphere

105

What does the lithosphere consist of

The crust and the rigid upper section of the mantle

106

How thick is the lithosphere approximately

80-90km thick

107

What is the lithosphere divided into

Seven large plates and a number of smaller ones

108

What are the two categories tectonic plates are divided into

Oceanic and continental, depending on the type of material from which they are made

109

Where is the asethenosphere

Lies beneath the lithosphere and is semi-molten on which the plates float and move

110

What is the thickness, age, density and composition of continental crust

30-70km
Over 1,500 million years
2.6 (lighter)
Mainly granite; silicon, aluminium, oxygen (SIAL)

111

What is the thickness, age, density and composition of oceanic crust

6-10km
Less than 200 million years
3.0 (heavier)
Mainly basalt; silicon, magnesium; oxygen (SIMA)

112

What is the basic earth structure

The inner core is solid and 5,100 km.
The outer core is liquid and 2,900km.
The mantle has 3 parts and includes the asthenosphere.
Crust 0-100km thick.
Lithosphere (crust and uppermost mantle)

113

What are the names of the tectonic plates

Eurasian plate.
Indo-Australian plate.
Pacific plate.
North American plate:
Nazca plate.
South American plate.
African plate.
Antarctic plate

114

Describe the tectonic plates and their margins

The Eurasian plate contests of most of Europe and Asia (including Indonesia) and runs through Iceland as the mid-Atlantic ridge. It is on a convergent (destructive, subduction zone) fault line with the indo-Australian plate which surrounds India, Australia, Papua New Guinea and runs through New Zealand.
They both are on convergent (destructive, subduction zones) boundaries to the Pacific plate, which is all oceanic.
This has a transform fault and is divergent (constructive, sea floor spreading) boundary with the Antarctic plate.
The nazca plate lies between the Pacific plate, the Antarctic plate, the North American plate and the South American plate.
The nazca is divergent (constructive sea floor spreading) next to the Pacific, it is convergent (destructive) next to the South American plate.
The North American plate consists of North America and a small part of russia.
It forms a conservative zone with the Pacific plate and a divergent (constructive) boundary next to the Eurasian plate.
The South American plate is a convergent (destructive) boundary next to the African plate which is divergent (constructive) to the indo-Australian plate.

115

Where is the mid-Atlantic ridge

Runs between South America, Africa and North America and Europe, straight through Iceland

116

Where are the oceans

North Pacific Ocean by North America and Asia.
South Pacific Ocean by South America and Australasia.
North Atlantic Ocean between North America and Europe.
South Atlantic Ocean by South America and Africa.
Southern Ocean by Antarctica.
Indian Ocean between Africa and Australia.
Arctic Ocean above Asia by the Arctic.

117

When maps of The Atlantic Ocean were first produced what did people notice

That the continents either side seemed to fit together remarkably well - the bulge of South America fitting into the indent below west Africa

118

Who noted the fact that the continents seem to fit together in the seventeenth century

Francis Bacon

119

Why did Francis Bacon not attract any serious attention

No one thought the continents could move

120

In 1912 who published the theory of a single continent existing 300 million years ago

Alfred Wegener

121

What did Alfred Wegner publish

The theory of Pangea that existed 300 million years ago.
He maintained that it later split into the two continents of Laurasia in the north and Gondwanaland in the south.
It was the theory of continental drift and claimed it was supported by several pieces of evidence that these areas were once joined.

122

What are the3 bits of geological evidence for the theory of continental drift

The fit of South America and west Africa.
Evidence of a late-Carboniferous glaciation (290 million years ago).
Rock sequences in northern Scotland closely agree with those found in eastern Canada.

123

Where were deposits of evidence of a late-Carboniferous glaciation found

In South America, Antarctica and India.
There were also striations on rocks in Brazil and west africa.

124

How is the evidence of a late-Carboniferous glaciation evidence for the theory of continental drift

The formation of these deposits cannot be explained by their present position; they must have been formed together and then moved.

125

How can the rock sequences in Scotland and Canada be used as evidence for continental drift

It indicates that they were laid down under the same conditions in one location

126

What are the 3 pieces of biological evidence for the theory of continental drift

Fossil brachiopods found in Indian limestone are comparable with similar fossils in Australia.
Fossil remains to the reptile Mesosarus are found in both South America and Southern Africa.
Fossilised remains of a plant.

127

Why is the fossil remains of the reptile Mesosaurus being found in South America and Southern Africa evidence for the theory of continental drift

It is unlikely that the same reptile could have developed in both areas or that it could have migrated across The Atlantic

128

How does the fossilised remains of a plant act as evidence of the theory of continental drift

The fossilised remains of a plant which existed when coal was being formed have been located only in India and Antarctica

129

Why did Wegeners ideas gain little ground

Because they were unable to explain how continental movement took place

130

When did evidence begin to accumulate to show that Wegeners theory could have been correct

1940s onwards

131

What was discovered in the 1940s that gives evidence of continental drift

The mid-Atlantic ridge was discovered and studied with a similar feature in the Pacific Ocean. Examination suggested that sea-floor spreading was occurring.

132

What is the evidence for sea-floor spreading in the mid-Atlantic ridge

The alternating polarity of the rocks that form the oceanic crust

133

How do magnetic ‘stripes’ in The Atlantic Ocean floor occur

Iron particles in lava erupted in the ocean floor are aligned with the earths magnetic field. As the lavas solidify these particles provide a record of polarity at the time of eruptions. However the earths polarity reverses at regular intervals. This results in a series of magnetic ‘stripes’ with rocks aligned alternately towards the north and south poles.

134

How often does the earths polarity reverse

Approx every 400,000 years

135

What is the record of the earths polarity at times of eruptions called

Palaomagnetism

136

Where is the striped pattern of magnetic ‘stripes’ found

Mirrored exactly on either side of a mid-oceanic ridge

137

What does the magnetic ‘stripes’ on either side of a mid-oceanic ridge suggest

The oceanic crust is slowly spreading away from this boundary

138

Beside the magnetic ‘stripes’ on either side of mid-oceanic ridges, what else helped to develop the theory of continental drift

The fact that oceanic crust gets older with distance from the mid-oceanic ridge

139

What does sea-floor spreading imply

That the earth must be getting bigger, as this is not the case however it must be that plates are being destroyed somewhere to accommodate the increase in their size at mid-Oceanic ridges

140

What is evidence that plates are being destroyed to accommodate the growth from constructive sea-floor spreading

The discovery of huge oceanic trenches where large areas of ocean floor were being pulled downwards in a process known as subduction

141

Describe the process of constructive plate boundaries

Hot spots around the core of the earth generate thermal convection currents within the asthenosphere, this causes magma to rise towards the crust and then spread before cooking and sinking. This circulation of magma is the vehicle upon which the crustal plates move.

142

What can crust be thought of doing

Floating on the denser material of the asthenosphere

143

What are constructive boundaries

Plates moving away from each other - divergent

144

What are destructive boundaries

Plates moving towards each other - convergent

145

What is a conservative plate boundary

Where two crustal plates slide past each other and the movement of the plates is parallel to the plate margin

146

Why is there volcanic activity at conservative margins

There is no subduction

147

What 5 landforms are associated with plate movements

Ocean ridges
Rift valleys
Deep sea trenches
Island arcs
Young fold mountains
Volcanoes

148

How are Ocean ridges formed

When plates move part in oceanic areas. The space between the plates is filled with basaltic lava upwelling from below to form a ridge.

149

What is the longest continuous uplifted form on the surface of the planet

Ocean ridges

150

What can form on ocean ridges

Volcanoes - submarine volcanoes which sometime rise above sea levels

151

Example of submarine volcano that rose above sea level

Surtsey to the south of Iceland

152

When do rift valleys form

When plates move apart on continental areas. The crust fractions as the plate moves apart and the broken crust drop down between parallel faults to form the ridge

153

Example of Rift Valley

In East Africa, the brittle crust fractures as sections of it move apart

154

What is a Horst

An area between two parallel rift valleys hat forms an upstanding block

155

What is the line of the African rift thought to be

An emergent plate boundary

156

What is an emergent plate boundary in Africa

The beginning of the formation of a new ocean as Eastern Africa splits away from the remainder of the continent

157

How do deep sea trenches form

Where oceanic and continental plates meet, the denser oceanic plate is forced underneath the lighter continental one (subduction).
The downwarping of the oceanic plate forms a very deep part of the ocean known as a trench.

158

Example of a deep sea trench

Off the western coast of South America, the Nazca plate is subducted under the South American plate forming the Peru-chile trench

159

Example of a deep sea trench formed by two oceanic plates

On the western side of the Pacific Ocean, the Pacific plate is sub-ducted beneath the smaller Philippine plate forming the very deep Marianas trench

160

How do Island arcs form

During subduction, the descending plate encounters hotter surroundings, and this coupled with the heat generated from friction, begins to melt the plate. As this material is less dense than the surrounding asthenosphere, it begins to rise towards the surface as plutons of magma. Eventually these reach the surface and form complex, composite and explosive volcanoes. If the eruptions take place offshore, a line of volcanic islands forms. These are known as island arcs.

161

Examples of island arcs

The Mariana’s islands and Guam form a good example, running parallel to the Marianas trench.

162

How do young fold mountains occur

The plates forming continent crust have a much lower density than the underlying layers so there is not much subduction when such plates meet. As such plates move towards each other, their edges and sediments between them are forced up into fold mountains

163

Why is there no volcanic activity near fold mountains

Because there is little subduction

164

How are deep mountain roots created

During the process of forming fold mountains, some material is forced downwards

165

Examples of young fold mountains

The previous intervening Ocean, known as the Sea of Tethys, has had its sediment forced upward in large overfolds to form the Himalayas, a process which is continuing today.

166

Currently, where is it likely the next set of fold mountains will occur in the future

The indo-Australian plate is moving northwards into the Eurasian plate

167

Why can sediment that has accumulated on the continental shelf, along the edge of a plate, be uplifted

As the plate edges buckle during the subduction of a denser oceanic plate

168

Examples of where subduction causes fold mountains

The Andes, running down the area where the nazca plate is being subducted beneath the lighter South American plate. This is because sediment that accumulates in the continental shelf can be uplifted

169

What causes a number of explosive volcanoes in the Andes

Molten magma rising from the depths

170

For a long time the generally accepted view of plate motion was convection currents. What is now believed

That forces behind plate motions are not as simple as would be explained entirely by convection currents

171

How can different forces, that aren’t convection currents, work on plate boundaries

These forces can push from the ridge, drag the plates down at the trenches, or act along the sides of plates at conservative boundaries

172

What does the force ‘ridge push’ occur

At constructive boundaries, the upwelling of got material at ocean ridges generates a buoyancy effect that produces the ocean ridge which stands some 2-3km above the ocean floor. Here, oceanic plates experience the force that acts away from the ridge

173

What is ridge push the result of

Gravity acting down the slope of the ridge

174

What indicates there is some frictional resistance to the force ‘ridge push’

The occurrence of shallow earthquakes, resulting from the repeated tearing apart of the new-formed crust

175

What do some experts prefer ‘ridge push’ to be called

The process ‘gravitational sliding’

176

What is the force ‘slab pull’

The situation at destructive plate boundaries. A major component is the downward gravitational force acting on the cold and dense descending plate as it sinks into the mantle. This gravity-generated force pulls the whole oceanic plate down as a result of the negative buoyancy of the plate. This is called ‘slab pull’

177

What happens due to the pushing of the sub-ducting plate through slab pull against the overriding plate

There is frictional resistance that gives rise to both shallow and deep earthquakes in subduction zones

178

What does the fact that each plate moves at its own rate suggest

That the relative importance of the driving and retarding forces must vary from plate to plate. It is therefore unlikely that any single agent is the sole driving mechanism of plate motion; plates are therefore controlled by a combination of forces

179

What are lahars

There are formed by volcanic ash mixing with water and flowing downhill. Essentially they are volcanic mudflows

180

Examples of where lahars can occur

In the Philippines if a typhoon occurs after a volcanic eruption, then lahars can be the result

181

What is lava

Molten rock (magma) flowing onto the surface. Acid lava solidifies very quality but basic lava (basaltic) tends to flow some distance before solidifying

182

Example of a place with basic lava

On the Hawaiian islands

183

What is the lithosphere

The layer of the earth which consists of the crust and the upper section of the mantle. It is this layer which is split into a number of tectonic plates

184

What are pyroclastic flows also known as

Nuées Ardentes

185

What are pyroclastic flows

Formed from a mixture of hot gas (over 800*C) and tephra. After ejection from the volcano they can flow down the sides of a mountain at speeds of over 700km per hour. Some volcanologists apply the term nuées ardentes when the cloud is formed int from hot

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What is tephra

The solid matter ejected by a volcano into the air. It ranges from volcanic bombs (large) to ash (fine)

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What is most volcanic activity associated with

Plate tectonic processes

188

Where are most volcanic activities located

Along plate margins

189

Where 4 places is volcanic acidity found

Along oceanic ridges.
One or near subduction zones.
Associated with rift valleys.
Over hot spots.

190

Why are volcanoes found along ocean ridges

Because the plates are moving part and magma is forcing its way to the surface, cooking and forming new crust.

191

What is Sea-floor spreading

As plates move far apart, the new crust is carried away from the ridge

192

Best example of nature and distribution of volcanoes along ocean ridges

The mid-Atlantic ridge where Iceland represents a large area formed by volcanic activity.
Volcanoes formed here have fairly gentle sides because of the low viscosity of the basaltic lava.
Eruptions are frequent but relatively gentle (effusive).
E.g Eyjafajallajökull.

193

What are eruptions that are frequent but relatively gentle called

Effusive

194

What are the components in a cross section of the mid-Atlantic ridge

Asthenosphere.
Lithosphere.
Oceanic crust.
Transform fault.
Central rift.
Sea level.

195

How do volcanoes form on or near subduction zones

The deeper the oceanic plate descends, the hotter the surroundings become. This, together with the heat generated form friction, begins to melt the oceanic plate into magma in part of the subduction zone known as the Benoit zone. As it is less dense than the surrounding material, this molten magma begins to rise as plutons of magma. Eventually they reach the surface and create composite and explosive volcanoes.

196

What is the Benioff zone

The part of the subduction zone where the oceanic plate begins to melt

197

What is the ring of fire

The line of volcanoes that surround the Pacific Ocean associated with plate subduction

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What are volcanoes on subduction zones composite and explosive

Because of the andesitic lava

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What is the nature of andesitic lava

Viscous (flows less easy)

200

What is the lava type of volcanoes on constructive margins

Basaltic (less viscous)

201

How do island arcs appear

If the eruptions in subduction zones take place offshore

202

Which plates are creating island arcs on the western side of the Pacific Ocean

The Pacific plate is being dragged beneath the smaller Philippines plate - the Guam and the Marianas have been formed form magma upwelling form the Benioff zone

203

What landforms are there near subduction zones

Trench
Marginal geosyncline
Mountain chains
Volcanoes

204

How do volcanoes form in rift valleys

When the areas of crust drop down between parallel faults to form the Rift Valley. The crust here is much thinner than neighbouring areas, suggesting that tension in the crust is causing the plate to thin as it starts to split. Through this thinning crust, magma forces its way up to the surface to form volcanoes.

205

Example of a volcano on a Rift Valley

Mt Nyiragongo

206

What causes a hot spot to develop

A concentration of radioactive elements below the crust

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What is a hot spot

Small area of earths crust where an unusually high heat flow leads to volcanic activity

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Where are hot spots located

Away from plate boundaries - creating a challenge for plate tectonic theory

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Example of hot spot volcanoes

Hawaiian islands (kauai is the oldest at 3.8 million years and Hawaii is the active, Liohi underwater volcano will eventually form the next succession)

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How do hot spot volcanoes form

A plume of magma rises from the core of the hot spot. This creates a column of upwelling lava which breaks through the surface causing an active volcano to form.

211

What volcanoes are created at hot spots

Huge (but relative to the area) flattish volcanoes called shield volcanoes

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How is a succession of volcanoes in hot spots formed

The hot spot is stationary so as the plate moves over it, a line of volcanoes is created. (Volcanic island chain)

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How do the oldest volcanoes in an island chain become seamounts below the level of the ocean

Because they had put so much pressure on the crust that subsidence has occurred. This, together with marine erosion replacing eruptions as the dominant process, causes them to get smaller

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In a hot spot volcanic chain, why may a volcano that’s not directly above the mantle plume still erupt

As the plate moves it drags the head of the thermal plume with it

215

Examples of volcanic eruptions having an enormous variation

They can involve the tranquil effusion of a sluggish lava; one the other hand they can take the form of huge explosions that eject gas and dust and can blot out the sun for many years, bringing on global climatic change

216

What is the main measurement of magnitude of volcanoes

The volcanic explosively index (VEI)

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What is the volcanic explosively index (VEI)

A logarithmic scale from 0 to 8.
Quiet lava-producing eruptions score 0-1 on the index whereas the more colloidal eruptions are nearer the high end.
9-8 eruptions occur very infrequently

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What was the VEI of the eruption of Mr St Helen’s and Pinatubo

5 and 6

219

What do volcanologists estimate the last eruption at 7 in the VEI was

Tambora (Indonesia) in 1815

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When was the last eruption which graded 8 on the VEI

73,000 years ago in Toba (indionesia)

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What do critics of the VEI point out

It does not take into account gas emissions or the atmospheric/climatic impact of eruptions

222

How do volcanologists determine the frequency of eruptions of specific volcanoes

It’s previous history of activity can be interpreted by volcanologists using the deposits associated with the volcano itself and those within the wider region it can effect

223

Where the effects a volcanic event range from

The area immediately around the volcano to the whole planet

224

What can the impact presented by a volcanic eruption be categorised into

Primary and secondary education

225

What are primary effects in a volcanic eruption brought about by

Material ejected from the volcano

226

What are the four primary effects of a volcanic eruption

Tephra
Pyroclastic flows
Lava flows
Volcanic gases

227

What is the global distribution of active volcanoes

Mostly around plate boundaries, especially the Pacific ring of fire and on the Mid-Atlantic ridge in Iceland. The SAN Andreas fault in North America also has a few.
One volcano in the middle of northern Russia and one in the middle of the Pacific Ocean, not on a fault. One in Africa on the west coast.

228

Example of a pyroclastic flow destroying a city

The Roman City of Pompeii (Italy) was destroyed in 79 AD From flows from Mt Vesuvius

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What are volcanic gases

Carbon dioxide, carbon monoxide, hydrogen sulphide, sulphur dioxide and chlorine.

230

Example of volcanic gases killing people

In 1989, carbon dioxide emissions from the lake in the crater of Nyos (Cameroon) killed 1,700 people

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What are the 6 secondary effects of volcanic eruptions

Lahars
Flooding
Volcanic landslides
Tsunamis
Acid rain
Climatic change

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What are lahars

Volcanic mud flows. Melted snow and ice as a result of the eruption combined with volcanic ash forms mud flows that can move down the course of river valleys at high speeds

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Example of lahar

In 1985, a lahar restores the Colombian town of Armero after an eruption of the volcano Nevado del Ruiz. Only a quarter of the 28,000 population survived

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How is flooding a secondary effect of a volcanic eruption

When an eruption melts glaciers and ice caps, serious flooding can occur

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Example of flooding after a volcanic event

In Iceland in 1996 when the Grimsvotn volcano erupted

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How are tsunamis a secondary effect of volcanic eruptions

Sea waves can be generated by violent eruptions

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Example of a tsunami as an effect of an eruption

In 1883, Tsunamis after the eruption of Krakatoa (Indonesia) killed 36,000

238

How is acid rain a secondary effect of volcanic eruptions

Volcanoes emit gases which include sulphur. When this combines with atmospheric moisture, acid rain occurs

239

How is climatic change a secondary effect of a volcanic eruption

The ejection of huge amounts of volcanic debris into the atmosphere can reduce global temperatures and is believed to have been an agent in past climatic change

240

When do volcanic events become hazardous

When they impact upon people and the built environment, killing and injuring people, burying and collapsing buildings, destroying infrastructure and bringing agricultural and other economic activities to a haunt

241

Why isn’t prediction a great management strategy of volcanic hazards

It’s difficult to predict when activity will take place.

242

How can prediction be a management strategy of volcanic hazards

A study of the previous eruption history of any volcano is important, along with an understanding of the type of activity produced.

243

What are the ways in which volcanologist are seeking to give accurate timings of an eruption

The monitoring of land swelling, changes in the groundwater levels and the chemical composition of groundwater and gas emission. It is also possible to monitor seismic activity looking for the shock waves that result from magma moving towards the surface, expanding cracks and breaking through other areas of rock

244

What does protection mean as a management of a volcanic hazards

Preparing for the event

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How is protection a management of a volcanic hazard

Monitoring a volcano will possibly identity a time when the area under threat should be evacuated. The government of several counties with volcanoes, such as New Zealand, have made risk assessments and from them produced a series of alert levels in order to warn the public of the threat

246

What provides evidence for hazard assessment as a management strategy of volcanic hazards

Geological studies of the nature and extend of deposits from former eruptions and associated Lahars and floods

247

What do hazard assessments allow to happen in the management of volcanic hazards

They allow for the identification of areas at greater risk and land use planning can be applied to avoid building in high risk areas

248

Examples of protection strategies for managing volcanic hazards

Once the lava has started to flow and is fairly viscous, it may be possible to divert it from the built environment.
On Mt Etna in Italy: digging trenches, dropping blocks into the lava steam and using explosives have been successful in slowing down the flow.

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Why do many devastated areas in poorer counties require aid for considerable periods of time after a volcanic hazard

Volcanic events can be prolonged and very damaging to the local economy

250

Why do many counties need aid after a volcanic hazard

Aid is needed for monitoring, evacuation, emergency shelters and food, long-term resettlement of the population and the restoration of the areas economic base and infrastructure

251

What are immediate responses to volcanic hazards

Those which take place just before or after the volcanic event such as warnings, evacuation and attempts to stop lava flows

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What do long term responses of volcanic hazards include

The monitoring of a volcano, research into finding new methods of prediction and even building barriers in anticipation of the direction of lava flows and Lahars

253

What is an earthquake

As the crust of the earth is constantly moving, there tends to be a slow build up of stress within the rocks. When this pressure is released, parts of the surface experience, for a short period, an intense shaking motion - an earthquake

254

What is retrofitting

In earthquake prone areas building and other structures can be fitted with devices such as shock absorbers and cross-bracing to make them more earthquake proof

255

What is a tsunami

Giant sea waves generated by shallow-focus underwater earthquakes, violent volcanic eruptions, underwater debris slides and landslides into the sea

256

What is the focus of an earthquake

The point at which this pressure release occurs within the crust

257

What is the epicentre

The point on the earths surface immediately above the focus of an earthquake

258

What are the three broad categories of earthquakes

Shallow focus (0-70km deep) - these tend to cause the greatest damage
Intermediate focus (70-300 km deep)
Deep focus (300-700km)

259

What percentage of all the earthquake energy released is caused by earthquakes with shallow focus’

75%

260

Where does the most damage in an earthquake occur

The nearer to the epicentre

261

What is sent out during an earthquake

Shock waves

262

Where do the vast majority of earthquakes occur

Along plate boundaries

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Where do the powerful earthquakes occur

Destructive marine

264

At conservative margins how are earthquakes created

The boundary is marked by a fault, movement along which produces the earthquake

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What is the most famous conservative margin that creates earthqkadsn

San Andreas fault in California, which represents the boundary between the North American and Pacific plates. In reality the San Andreas system consists of a barrier complex zone in which there are a number of fractures of the crust

266

What are some earthquakes associated away from plate boundaries associated with

The reactivation of old fault lines

267

What has been suggested as the cause of some minor earthquakes

Human activity

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How can human activity cause minor earthquakes

Through building large reservoirs which puts pressure on the underlying rocks, or subsidence of deep mine workings.

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What is the global distribution of earthquakes

Around plate boundaries (ring of fire, mid Atlantic ridge, San Andreas fault) and some midland of the Eurasian plate, African plate, Pacific plate.

270

In recent times, what have people been worried about

The process of fracking (hydraulic fracturing of rock in order to release gas)

271

What are the ways in which the magnitude of earthquakes is measured

The Richter scale
The moment magnitude scale (MMS)
The Mercalli scale

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What is the Richter scale

A logarithmic scale - an event measured at 7 in the scale has an amplitude ten times greater than one measured 6 on the scale. Energy release is proportional to the magnitude, so that for each unit increase on the scale, the energy released increases by approximately 30 times

273

Why do some geologists use the moment magnitude scale now

Because they have been unhappy with the fundamentals of the Richter scale for some time

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What does the MMS identify

Energy release. It’s scale is the same as that of the Richter 1-10.

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What was the largest earthquake ever recorded by the MMS

The Valdivia (Chile) event in 1960 at 9.5 MMS

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Examples from the Richter scale

1-3 : normally only detected by seismographs, not felt.
4: faint tremors causing little damage.
5: widely felt, some structural damage near epicentre.
6: distinct shaking, less well-constructed buildings collapse.
7: major earthquake causing serious damage.
8: great earthquake causing massive destruction and loss.
9-10: very rare great earthquake causing major damage over a large region and ground seen to shake.

277

What does the mercalli scale measure

The intensity of an event and its impact. It is a 12-point scale where level 1 is approximate to 2 on the Richter scale. It goes up to level XII (approximately 8.5 on Richter)

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What are some examples of the mercalli scale according to the USGS

I: not felt (not felt except by a very few under especially favourable conditions)
II: weak (felt only by a few)
III: weak (felt quite noticeably by persons indoors, vibrations)
IV: light (felt indoors by many and outdoors by few, dishes, windows, doors disturbed)
V: moderate (felt by nearly everyone, some dishes and windows broken)
VI: strong (felt by all, many frightened. Damage slight)
VII: very strong (damage negligible in buildings of good design and construction)
VIII: severe (damage slight in specially designed buildings. Considerable damage in normal buildings)
IX: violent (damage considerable in all buildings)
X: extreme (buildings destroyed, rails bent)
XII: extreme (bridges destroyed, underground pipeline completely out of service)
XIII: extreme (damage total, waves seen on ground surface, lines of sight and level distorted, objects thrown upwards in air)

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What do seismic records enable

Earthquake frequency to be observed

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What is a fault of seismic records

They only date back to 1848 when an instrument capable of recording seismic waves was first developed. Before that we have to consult historical records as to the date and the effects of the identical event

281

What are the primary effects (impacts) of an earthquake

Ground shaking
Ground rupture

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What does the severity of ground shaking depend upon

The magnitude of the earthquake, it’s depth, the distance form the epicentre and the local geological conditions

283

What were the seismic waves that devastated Mexico City in 1985 amplified by

The ancient lake sediments upon which the city is built

284

What is ground rupture

The visible breaking and displacement of the earths surface, probably along the line of the fault

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What does ground rupture pose a major risk for

Large engineered structures such as dams, bridges and nuclear power stations

286

What are 5 secondary effects of seismic hazards

Soil liquefaction
Landslides/avalanches
Tsunamis
Fires
Effects on people and the built environment

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How is soil liquefaction a secondary effect of seismic hazards

When violently shaken, soils with a high water content loses their mechanical strength and start to behave like a fluid

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How are landslides/avalanches a secondary effect of seismic hazards

Slope failure as a result of ground shaking

289

How are tsunamis a secondary effect of seismic hazards

Giant sea waves generated by shallow-focus underwater earthquakes involving movements of the sea bed, or landslides into the sea

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How are fires a secondary effect of seismic hazards

They result from broken gas pipes and collapsed electricity transmission systems

291

Examples of the effects on people and the built environment being a secondary effect of seismic hazards

Collapsing buildings; destruction of road systems and other forms of communication; destruction of service provisions such as water, electricity and gas; flooding; disease; food shortages; disruption to the local economy, either subsistence or commercial.

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What will some of the effects on the human environment from seismic hazards depend on

The ability of the area to recover

293

What are the characteristics of tsunamis

Very long wavelength (sometimes over 100km)
Low wave heigh (under one metre) in the open ocean
Travel at speeds of over 700km per hour

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How long do some tsunamis take to cross the Pacific Ocean

Less than a day

295

What happens to tsunami waves when they reach shallow water bordering land

They increase rapidly in height

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What is the first warning given to coastal populations about an oncoming tsunami

The wave trough in front of the tsunami which results in a reduction in sea level, known as a drawdown.
Behind this comes the tsunami itself.

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How high can tsunamis reach

An excess of 25m

298

What do tsunami events usually consist of

A number of waves, the largest not necessarily being the first

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How far did the Indian Ocean tsunami reach

Started in the West coast of Indonesia and spread through Kenya, bangladesh and throughout the whole of Indonesia

300

When a tsunami reaches land, what 5 things will it’s effect depend upon

The height of the waves and the distance they have travelled.
The length of the event (at source).
The extent to which warnings could be given.
Coastal physical geography, both offshore and on the coastal area.
Coastal land use and population density.

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What are some effects of tsunamis

The wave will wash boats and wooden coastal structures inland, and the backwash may carry them out to sea. People are drowned or injured by the tsunami as both the water itself and the debris that it contains are hazards. Buildings, roads, bridges, harbour structures, trees and even soil are washed away.

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What do most tsunamis have an effect on depending upon the coastal geography

At least 500-600m inland

303

What percentage of all tsunamis are generated within the Pacific basin

Around 90%

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What are the tsunamis in the Pacific basin associated with

The tectonic activity taking place around its edges

305

What plate boundaries generate the most tsunamis

Convergent plate boundaries where subduction is taking place, particularly on the western side of the Pacific and the bordering eastern side of the Indian Ocean

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What percentage of all tsunami events take place on the eastern side of the Indian Ocean

25%

307

Which areas do the geological record indicate that huge tsunamis have affected

The Mediterranean Basin (the Santorini eruption around 1450 BC) and the North Sea (for example the Storegga slide, around 7240 BP) resulting from huge submarine debris slides off Norway which produced tsunamis of over 6m in height in Scotland and other areas bordering the North Sea. It is believed these tsunamis continued across The Atlantic to hit the coastlines of Spitsbergen, Iceland and Greenland

308

What are the 3 ways to manage seismic hazards

Prediction
Prevention
Protection

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What is the prediction of earthquakes

Very difficult

310

How can regions at risk from seismic hazards be identified

Through plate tectonics, but attempts to predict a few hours before the event are questionable

311

What are attempts at prediction seismic hazards based upon

Monitoring groundwater levels, release of radon gas and unusual animal behaviour. Fault lines such as the Sans Andreas can be monitored and the local magnetic fields measured

312

How can producing a hazard zone map predict the impact of an earthquake

Areas can be mapped on the basis of geological information and studies made into ground stability. The map can be acted upon by local and even national planners

313

What can close studies of fault lines sometimes indicate

The point along the fault line where the next earthquake could be due

314

What did a study of the pattern of the seismic events along the San Andreas fault between 1969 and 1988 indicate

The existence of a ‘seismic gap’ in the area of Lona Prieta (that is, the area had not had any real seismic activity for the past 20 years)

315

When do seismic surveys not work

For events which take place on unknown fault lines

316

What is trying to prevent an earthquake thought to be

Almost impossible

317

Some studies have looked at the feasibility of schemes to keep plates sliding past each other (rather than sticking and then releasing) as a management of a seismic hazard, what are some examples

Lubricating the movement by focusing on water and oil. Some have even gone as far to suggest nuclear explosion

318

Why is it essential for everyone from civil authorities to individuals to be prepared for a seismic hazard

Since earthquakes strike suddenly, violently and without warning

319

Example of a programme to protect places from seismic hazards

In the USA, the Federal Emergency Management Agency (FEMA)

320

What are the 4 objectives of FEMA

To promote understanding of earthquakes and their effects.
To work to better identify risk.
To improve earthquake-resistant design and construction techniques.
To encourage the use of earthquake-safe policies and planning practices.

321

What does protection from a seismic hazard mean

Preparing for the event by modifying the human and built environment in order to decrease vulnerability. Includes attempts to modify the loss by insurance and aid.

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What are the 8 ways to protect a place as a management of a seismic hazard

Hazard-resistant structures
Education
Fire prevention
Emergency services
Land-use planning
Insurance
Aid
Tsunami protection

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How can hazard resistant structures be used as management of a seismic hazard

Buildings can be designed to be aseismic, in that they can be earthquake resistant

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What are the three main ways that buildings can be designed to be aseismic

By putting a large concrete weight on top of the building which will move, with the air of a computer programme, in the opposite direction to the force of the earthquake in order to counteract stress.
Putting large rubber shock absorbers in the foundation which will allow some movement of the building.
By adding cross-bracing to the structure to hold it together better when it shakes.

325

What can happen to older buildings and structures, such as elevators and motor ways, to make them more earthquake proof

They can be retrofitted with devices

326

Example of a comparison which shows the effects of different types of buildings on earthquakes

Comparison between the 1989 Loma Prieta earthquake (6.9 MMS) and the 1988 event in Armenia (6.8 MMS).
Greater earthquake proof buildings of California resulted in 63 deaths whereas in Armenia, over 25,000 people died, many buildings collapsed as a result of soft foundations and no earthquake proof features.

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For many areas what’s the main way that loss of life from seismic events can be minimised

Education

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How does education help protect from a seismic event as a management strategy

Instructions are issued by the authorities in how to prepare for such events by securing homes, appliances and heavy furniture, and assembling ‘earthquake kits’.

329

Example of education as a management strategy for seismic events

Children having earthquake drills at school as do people in offices and factories.

330

How does fire prevention help protect from a seismic event as a management strategy

‘Smart metres’ have been developed that can cut off the gas if an earthquake of sufficient magnitude occurs.

331

What do emergency services need

Careful organisation and planning

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How do emergency services help protect from a seismic event as a management strategy

Heavy lifting gears need to be available and many people should be given first aid training, as it could be some time after the event that trained medical personnel arrive. Much of the preparation in California involves the establishment of computer programs that will identity which areas the emergency services should be sent to first

333

How does land use planning help protect from a seismic event as a management strategy

The most hazardous areas in the event of an earthquake can be identified and then regulated in terms of land use. Certain types of buildings should be put in areas of low risk, such as schools and hospitals. It’s also important to have sufficient open space, as this forms a safe area away from fires and aftershock damage to buildings

334

How does insurance help protect from a seismic event as a management strategy

In richer areas, people are urged to take out insurance to cover their losses, the only problem being that for individuals, that is expensive. In the Kobe earthquake in Japan in 1995 only 7% of the people were covered by earthquake insurance

335

How does aid help protect from a seismic event as a management strategy

Most aid to poorer countries has generally been to help in the few days after the event, providing medical services, tents, water purification equipment, search and rescue equipment etc.

336

Why is aid over the long term problematic

Because it is something which is needed for the reconstruction of the built environment and redevelopment of the economy

337

How does tsunami protection help protect from a seismic event as a management strategy

They cannot be entirely predicted, even if the magnitude and location of an earthquake is known. Certain automated systems can be installed to give warnings, the best of which uses bottom pressure sensors, attached to buoys, which constantly measure the pressure of the overlying water column.

338

What do regions with a high tsunami risk use to warn people of a tsunami

Warning systems (such as a klaxon) to warn the population before the wave reaches the land

339

What is mitigation

Mitigation strategy is designed to reduce or eliminate risks to people and property from natural hazards. Money spent prior to a hazardous event to reduce the impact of it can result in substantial savings in life and property following the event

340

What is a storm surge

A rapid rise in sea level in which water is piled up against a coastline to a far excess of the normal conditions at high tide. Usually produced during the passage of a tropical storm when wind-driven waves pile up water against a coastline combined with the ocean bracing upwards as a result of much lower air pressure

341

What are tropical revolving storms (hurricanes, cyclones, typhoons)

Intense low-pressure weather systems that develop in the tropics, between the tropics of Cancer = 23* north and the tropical of Capricorn = 23* South. They are huge spinning storms with strong winds and torrential rain.

342

What is the usually diameter of tropical storms

200-700km

343

How do tropical revolving storms develop

They begin with an area of low pressure, resulting from surface heating, into which warm air is drawn in a spiralling manner. Such small-scale disturbances can enlarge into tropical depressions with rotating wind systems and these may continue to grow into a much more intense and rapidly rotating system - the tropical revolving storms.

344

What isn’t clear about the formation of tropical storms

Why they become so intense

345

What 5 conditions need to be present for a tropical storm develop

Oceanic location with sea temperatures above 27*C.
Ocean depth of at least 70m.
A location at least 5* north or south of the Equator.
Low level convergence of air in the lower atmospheric circulation system.
Rapid outflow of air in the upper atmospheric circulation.

346

What are the 3 different names for tropical storms

Hurricanes
Cyclones
Typhoons

347

Why is the condition of ‘Oceanic location with sea temperatures above 27*C’ needed for tropical cyclones to occur

It provides a continuous source of heat in order to maintain rising air currents

348

Why is the condition of ‘an ocean depth of at least 50m’ needed for tropical cyclones to occur

This moisture provides latent heat; rising air causes the moisture to be released by condensation and the continuation of this drives the system

349

Why is the condition of ‘a location at least 5* north or south of the equator’ needed for tropical cyclones to occur

Because this means the Coriolis force can bring about the maximum rotation of the air (the coriolis force is weak at the equator and will stop a circular air flow from developing so tropical storms don’t form between 0-5* north and south of the equator)

350

Why is the condition of ‘low level convergence of air in the lower atmospheric circulation system’ needed for tropical cyclones to occur

Winds have to come together near the centre of the low-pressure zone

351

Why is the condition of ‘rapid outflow of air in the upper atmospheric circulation’ needed for tropical cyclones to occur

This pushes away the warm air which has risen close to the centre of the storm

352

When does the tropical revolving exist

While there is a supply of latent heat and moisture to provide energy and low frictional drag on the ocean surface

353

How does the central eye of a storm develop

When the tropical revolving system reaches maturity

354

What is the central eye of a storm

An area 10-15km in diameter in which there are calm conditions, clear skies, higher temperatures and descending air

355

What have been observed around the eye of a storm

Wind speeds of more than 300km/hour

356

What is low pressure in an area

An area in which there is less air than in surrounding areas. This means that the air here rises because there is less air pressing down on it from above. Air moves from an area of high pressure to areas of low pressure. This movement of air is felt as wind.

357

What is the cyclonic flow

As the air rises, the water vapour within it condenses forming clouds and often precipitation too. Because of earths spin and the Coriolis effect, winds of a low pressure system swirl counterclockwise north of the equator and clockwise south of the equator - the cyclonic flow

358

Characteristics of tropical storms

Winds of 120km/he to over 250km/hr.
Torrential rain.
Circular in shape.
Hundreds of kilometres wide.
Usually last 7-14 days.
Develop over warm water (above 27*C)

359

What is the Coriolis effect

A force caused by the earths rotation. It reflects the path of the converging winds causing the winds to rotate.

360

Why do tropical storms loose strength when they move over land (landfall) or they reach colder waters polewards

As the source of heat and moisture is removed

361

Where provides the perfect condition for the formation of tropical storms

The Inter Tropical Convergence Zone (ITCZ) where two limbs of the Hadley cell converge to form low pressure on the ground

362

Once generated, where do tropical storms tend to move

Westwards

363

What is the distribution of tropical storms

In the Caribbean Sea/gulf of Mexico
On the western side of Central America
In the Arabian Sea/bay of Bengal
Off Southeast Asia
Off Madagascar
Off north western and north-Easten Australia

364

In the Caribbean Sea/ Gulf of Mexico what are tropical storms known as and what percentage of all tropical revolving storms occur here

Hurricanes and 11%

365

In the Western side of Central America (eastern Pacific) what are tropical storms known as and what percentage of all tropical revolving storms occur here

Hurricanes and 17%

366

In the Arabian Sea/bay of Bengal what are tropical storms known as and what percentage of all tropical revolving storms occur here

Cyclones and 8%

367

Off Southeast Asia what are tropical storms known as and what percentage of all tropical revolving storms occur here

Typhoons (1/3 of all storm events every year occur here)

368

Off Madagascar (Southeast Asia) what are tropical storms known as and what percentage of all tropical revolving storms occur here

Typhoons and 11%

369

Off northwest and northeaster Australia what are tropical storms known as and what percentage of all tropical revolving storms occur here

Willy-Willies and 20%

370

What is the magnitude of tropical storms measured on

The Saffir-Simpson scale

371

What is the Saffir-Simpson scale

A five point scale based upon central pressure, wind speed, storm surge and damage potential.

372

What does a scale 5 event on the Saffir-Simpson scale have

Central pressure at 920mb or below.
Wind speeds at 250km/hr or greater.
Storm surge at 5.5m or greater.
Damage potential that refers to ‘complete roof failure of many buildings with major damage to lower floors of all structures lower than 3 meters above sea level, evacuation of all residential buildings on low ground within 16-24km off coast is likely.

373

Every year how many tropical storms form

Around 80-100

374

What percentage of tropical storms go on to become a revolving tropical storm

80%

375

What 5 factors does the vulnerability of people to tropical storms depend upon

The intensity of the storm.
Speed of movement: the length of time over the area.
Distance from the sea.
Physical geography of the coastal area.
The preparations made by a community.
Warnings and community response.

376

How does the physical geography of the coastal area alter people’s vulnerability to tropical storms

Width of the coastal plain or size of delta, and location of any mountain ranges relative to the coast

377

Why do many tropical storms not develop into a hazard

They don’t reach land (don’t evolve into a revolving tropical storm)

378

When are storms more frequent in the northern hemisphere

Between June and novermber

379

When are tropical storms more frequent in the Southern Hemisphere

Between November and April

380

What is the impact wind from a tropical storm can have on an area

Scale 5 events can cause structural damage to buildings (even collapse) and roads, bridges etc. They can bring down electricity transmission lines and devastated agricultural areas. The huge amounts of debris that are flung about are a serious threat to people’s lives.

381

What is the impact heavy rainfall from a tropical storm can have on an area

They can bring about severe flooding, landslides and mudslides.

382

What can rainfall from a tropical storm exceed

200 to 300mm. If there is high relief near the coastal area, rainfall could increase over 500 mm/day

383

What is the impact storm surges from a tropical storm can have on an area

They can have devastating effect on low-lying coastal areas such as river deltas where the flooding can extend a long way inland.
They cause the majority of deaths in such events and agricultural areas can suffer for a long time as soil is contaminated by sea water.

384

What are the four ways of managing the tropical revolving storm hazard

Prediction
Prevention
Protection
Preparedness

385

What is wildfire a natural process in

Many ecosystems, it can be necessary and even beneficial

386

What does the prediction of tropical cyclones depend upon

The state of monitoring and warning systems

387

Example of a weather bureaux for tropical storms

The National Hurricane Centre in Florida (USA)

388

What do the USA do

They are able to access data from geostationary satellites and from both land and sea based recording centres. They maintain a round the clock surveillance of tropical storms that have the potential to become hurricanes by the use of weather aircraft

389

Why is information from weather bureaux useful

The information they collect can be compared with computer models so that a path can be predicted and people warned to evacuate an area

390

Why is it essential that information from weather bureaux correct

There is a high economic cost associated with evacuation, and as with all false alarms, people may become complacent and refuse future advice.

391

What is the estimation of cost to evacuate the coastal areas in the USA

One million dollars per kilometre of coastline due to losses in businesses and tourism and the provision of protection

392

Why is it not always possible to give more than 12-18 hours warning of cyclones

Because they tend to follow an erratic path

393

What does the fact that it's not always possible to give more than 12-18 hours of cyclones mean for poorer places

Where communications are poor, this is insufficient time for an evacuation

394

What have some high income places established to give people a chance to evacuate in case of a tropical storm

Warning systems

395

While tropical storms can't be prevented, what can be done

Research into the effect of cloud seeding in order to cause more precipitation. The theory is that if the cyclone could be forced to release more water over the sea, than this would result in a weakening of the system as it approaches land.

396

Why has research into cloud seeding to prevent cyclones not been continued

There was some concern expressed over the effects of this on the global energy system

397

What does 'protection' as a managment strategy of cyclones mean

Being prepared

398

What will predicting the landfall of a tropical storm enable

Evacuation to take place, together with the emergency services being put on full alert.

399

What happens if evacuation because of a cyclone does take place

Protection units, such as the National Guard in the USA, have to be called in to prevent homes and commercial properties from being looted.

400

Why are people made aware of how to strengthen their homes and properties in case of a cyclone

So they can withstand high winds

401

Example of cyclone/hurricane drill that is practiced

In Florida, 'Project Safeside' which is a hurricane awareness programme that is composed of precautionary drills for use in schools and the emergency operations centre of the state

402

What are the 5 ways protection as a management strategy of a cyclone occurs

Cyclone/hurricane drills
Land-use planning
Sea walls
Breakwaters
Flood barriers
Retrofitting

403

When storm surges are a problem because of cyclones what can be used to protect the area

Land-use planning which csn identify the areas at greater risk and certain types of development can be limited in such areas.

404

What can houses be put on to protect against flooding from a cyclone

Stilts

405

In the USA, how are local authorities required to address the problem of storm surges

By limiting expenditure on developments in high-risk areas and directing populations away from them, as well as having sound plans to reduce evacuation times and for post-disaster development

406

When does land-use planning not always work

In poorer areas where the need for land outweighs any considerations

407

How can some structures be retrofitted as a management of a tropical storm

By adjusting the buildings to make it resistant to wind to ensure greater safety during an event

408

What is a way people can use their abilities to mitigate the effects of tropical storms

Through preparedness

409

Examples of preparedness in Outerbanks

Local communities have got together to put into a practice the Outer Banks Mitigation Plan. It aims to make as much information as possible available to the people of the outer banks area

410

On the eastern seaboard of the USA, what is an area susceptible to the dangers brought by hurricanes

Part of the state of North Carolina, a group of barrier islands known as Outer Banks

411

What are the aims of the Outer Banks Mitigation Plan in managing tropical storms

It's aims are to save lives and money, property and natural resource protection, reduce future vulnerability, speedy recorders from the effects of hurricanes and post disaster funding.

412

Why is damage to the economic base of a poor area likely to last for years after a tropical storm

Becsuse, as with other phenomena, rich people are urged to take out insurance, whereas in poorer countries this is not always possible

413

What is important following a cyclonic event

That aid is available in the short term and long term

414

What do people's abilities to resist natural hazards depend upon

That aid is available in the short term and long term

415

Why do poorer areas suffer more because of natural hazards

Because land-use planning, warning systems, defences, infrastructure and emergency services are inadequate and this usually results in a higher death toll.
While not monetarily, the simple dwelling of the inhabitant of a poor country may suffer a huge loss, taking into account the time invested in it and the years of irreplaceable and uninsured savings that it represents.

416

How are richer counties better prepared in the case of a natural disaster

They have some planning systems in place, sophisticated warning arrangements, better defences and infrastructure and emergency services that are much more comprehensive

417

Why do HICs like the USA bear much greater monetary loss after a tropical storm event, even though they are better prepared

Becsuse of the damage to the built environment, however this damage is usually covered by insurance e.g house insurance

418

What are surface fires

Fires that sweep rapidly over the ground, consuming plant litter, grasses and herbs, and scorching trees, and it is possible for ground temperatures to rise over 1000*C

419

What are crown fires

Fires at a higher level than surface fires that spread through the canopy of trees

420

What does the nature of fire depend upon

The types of plants involved, strength of the winds, topography of the area in question and the behaviour of the fire itself

421

Once vegetation has dried out, what does the nature of fire largely depend on and why

The wind because wind drives the fire forward and burning embers that ignite more vegetation are more easily spread in windy weather

422

Where do the largest wildfires occur

In dry windy weather with low humidity

423

What are the 2 key factors in a fire

The climate and nature of the plants

424

What is a retardant

Chemicals sprayed on the fires in order to slow them down. They are composed of nitrates, ammonia, phosphates, sulphates and thickening agents

425

What is pyrophytic vegetation

Pyrophytes are plants adapted to tolerate fire. Methods of survival include thick bark, tissue with a high moisture content and underground storage structures

426

What 2 things are needed for a natural fire to occur

An ignition source
Fuel

427

What is the main ignition sources of natural wildfires

Lightning (electrical storms)

428

What affects the frequency of electrical storms

Climate, particularly when there is no rainfall

429

Where are fires that are the result of human intervention particularly situated

In and around settlements

430

How are human fires started

Falling power lines
Carelessly discarded cigarettes
Children playing with matches
Camp fires
Agricultural fires (controlled burning) which get out of hand
And in some cases arson

431

Which places have an increased danger of fires because of access to wild areas by tourists

The USA and Australia

432

What 2 conditions of fuel (wood) is needed for a wildfire

Sufficient quantity and dry enough to burn

433

How does fuel dry out to cause wildfires

Climate affects the frequency and duration of droughts during which the vegetation and litter has an opportunity to accumulate and dry out

434

How does climate affect the fuel of a wildfire

Affects the frequency and duration of droughts which dries out vegetation.
It also affects the type of vegetation that will grow in an area and the rate at which litter can be produced.

435

What kind of hazard are wildfires

A rural hazard

436

Where do wildfires occur

Most environments although with the continued expansion of human habitation, wildfires now occur within the boundaries of even substantial settlements

437

Where is the world do wildfires occur

California, Australia, Florida and the countries of Southern Europe like France, Italy, Greece, Turkey and Mediterranean islands duh as Sicily, Cyprus, Corsica and Sardina

438

Which areas are most susceptible to wildfires

Those with a combination of dry vegetation and lightning strikes.
Areas with a dry season are most likely to be affected as are those regions of the world with a semi-arid climate and susceptible to drought

439

Example of fires and natural ecosystems being linked

Mediterranean climate regions and the savannah grasslands

440

What are some good impacts of wildfires

They can clear vegetation and aid new seed germination, stimulate the growth of certain plants and rid of an area of insects and some parasites

441

examples of pyrophytic vegetation

Baobab tree has resistant bark.
In Australia, plants such as banksia need fire for their woody fruit to open and thus regenerate.

442

Why are fires not a real hazard of tropical rainforests

Due to the humid climate

443

What has recent burning for forest clearance in tropical rainforests that has gotten out of hand resulted in

Widespread fires that burned out of control for long periods

444

Which rainforests have suffered from fires in recent years

Amazon Basin (Brazil) and south-east Asia (Indonesia)

445

What is drought-resistant chaparral

Scrub vegetation

446

In Los Angeles what is the Santa Ana

A dry wind that descends from local mountains and increases the dryness of the vegetation to the point where a small spark can cause a major fire

447

What are the 6 primary effects of wildfires

Loss of crops, timber and livestock.
Loss of life.
Loss of property.
Realise of toxic gases and particulates.
Loss of wildlife.
Damage to soil structure and nutrient content.

448

How can the loss of crops, timber and livestock be an effect of wildfires

Forest fires can have a huge impact in timer producing areas, with the loss of trees taking many years to replace.

449

In the US what is the estimated price spent fighting wildfires

$10 million

450

How can the loss of life be an effect of wildfires

Although many fires are events from which people can get out of the way, some fires move so fast that people can be trapped although this is not usual

451

How many people lost their lives in the Victorian (Australia) bushfires of 2009

173 people

452

How can the loss of property be an effect of wildfires

At one time, only a few rural communities were at risk from fires, but with urban expansion, the fringes are now susceptible. The cost of damage and of fighting the fires can run into hundreds of millions of dollars. After such events, large numbers of people can be left homeless

453

How can the damage to soil structure and nutrient content be an effect of wildfires

With the intense heat generated at ground level, wildfires can destroy many soil nutrients and lead to an alteration in the soils structure

454

What are the two secondary effects of wildfires

Evacuation
Increased flood risk

455

How is evacuation a secondary effect of wildfires

Many people will flee from the area of the fire. Such people will not be allowed back into the affected area, often for a long period, if not forever. Emergency shelters/accommodation will have to be found along with food etc

456

How can the increased flood risk be an effect of wildfires

In certain environments, where rain comes in heavy bursts, the loss of so much vegetation, and the consequent decrease in interception, can lead to increased flooding

457

What are the 3 main ways of dealing with the fire hazard

Planning to mitigate the effect of an event.
Coping with the wildfires.
Addressing the effects.

458

What are the 7 in which the fire hazard can be managed before the event occurs

Managing the vegetation.
Managing the built environment.
Modelling.
Education.
Warning systems.
Community action.
Being well insured.

459

How is managing the vegetation a way to manage a wildfire before the event occurs

This is done by controlled burning to get rid of much of the litter and by creating firebreaks in the vegetation in advance rather than during the event

460

How is managing the built environment a way to manage a wildfire before the event occurs

This is done by increasing the gap between houses and vegetation and by incorporating more fire-resistant methods in construction (using more stone and brick rather than the wood; fitting spark arresters to chimneys)

461

How is modelling a way to manage a wildfire before the event occurs

This involves studying the ways in which fires behave with computer simulations in order to comprehend and predict fire behaviour

462

How is education a way to manage a wildfire before the event occurs

In areas susceptible to wildfires, it is important to make people aware with regards to home safety and how to avoid starting fires

463

How are warning systems a way to manage a wildfire before the event occurs

These can be put in place by establishing lookout towers and even air patrols. In tourist areas, notice boards at strategic locations could carry warnings of the fire hazard

464

How is being well insured a way to manage a wildfire before the event occurs

In wealthier counties, residents are urged to take out insurance against fire-damage, although this can be very expensive in fire-prone areas

465

What does the fire propagation model

The 'fire start.'
The 'propagation axis' (wind) goes through the middle.
The 'left front' is above the 'propagation axis' (wind).
The 'right front' is above the 'propagation axis' (wind).
The 'head of the fire' is at the end of the 'propagation axis'(wind)

466

What does dealing with the fire hazard event as it happens involve

Fighting the fires as they happen, which can be a very dangerous operation and it is not unknown for firefighters to suffer fatalities when they are involved in this action.

467

How do firefighters deal with wildfires

Spraying with water and chemicals from the ground and in the air (which can be costly).
They also work on the ground beating out the flames and bulldozing large breaks in the vegetation.
Retardants are also used.

468

How does firefighters beating flames and bulldozing large breaks in the vegetation help deal with wildfires

This prevents the fire jumping in certain directions

469

How do retardants deal with wildfire events

They flow the pace of the wildfire, they are often sprayed on fires in areas which are fairly inaccessible or when human safety and structures are endangered

470

Once the fire has been extinguished, what is needed

In the short term, communities and governments need to try and repair the damage caused by the fire.
In the long term, action will mean that attention will be directed towards making sure that areas are well prepared for the next fire.

471

What are the two ways of addressing the effects of wildfires

Replanting trees
Preparedness

472

What are the two ways that replanting trees address the effects of wildfires

Particularly in commercials forestry areas this improves the economy of areas devastated by fires.
After vegetation has been removed by fire, there is a great danger of flash flooding and mudslides on, what are now, unprotected slopes. Planting trees should stabilise slopes and should also lead to an improvement in water quality.

473

What does preparedness in address the effects of wildfires mean

This means making sure that people are better prepared for the next fire by having emergency supplies ready, along with survival kits, etc, and by setting up community groups such as that in Victoria.