Tectonics Flashcards

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1
Q

Why not all tectonic activity is hazardous?

A
  • low magnitude earthquakes
    -volcanic eruptions vary in terms of their explosivity due to location and lava type
  • good building design limits collapses
  • lack of population to be affected
    -high frequency of events allows people to prepare and respond avoiding death and minimising damage
    -accurate prediction allows efficient evacuation
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2
Q

PAR model

A

Shows a clear link between level of economic development in the root causes, leading to a progression of vulnerability,which then factors into hazard risk

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3
Q

How can hazard profiles aid effective management

A

-magnitude: most import factor in determining the success of modifying the event management strategies as most approaches cannot cope with Mega earthquake
-areal extent:vital factor as it determines the number of people affected but also the larger the are the more difficult it is for the existing emergency services to reduce loss of the earthquake event
-frequency:key factors in determining success of management as the more frequent the earthquake the more Likely the community is to be educated and aware of the hazard threat. Equally, low frequency can reduce the awareness of the hazard risk
- economic development:vital factor as it determines whether area can afford to implement all 3 types of strategies

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4
Q

Level of economic development

A

It refers to the broad socioeconomic status of a country: whether they recognise the hazard and have sufficient financial status to implement changes on national or local scales

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5
Q

Governance

A

The ability of an organisation/ group of people to plan or manage hazard events effectively.
Eg national government might finance emergency care, mandate education strategies or establish building regulations .
Local government night organise evacuation strategies.
Global governance might coordinate a tsunami warning system

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6
Q

What does level of economic development affect?

A
  • available capital
    -availability of resources
    -level of expertise and specialist equipment
    -quality of building design
  • quality of community preparedness -drills,education programmes
    -likelihood of insurance coverage
  • reliance on international assistance
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7
Q

What does governance relates to

A
  • ability to manage hazards
  • strength of regulations on building design
    -levels of corruption, so resource/capital availability
    -organisation of drills and evaluation strategies
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8
Q

What does the disaster risk- poverty nexus model seeks to establish

A

-poverty is both a cause and consequence of disaster impacts
-that repaired occurrence helps to sustain and maintain poverty in a region

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9
Q

Global interdependence

A

Relates to how interconnected places are

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10
Q

Japan 2011 case study

A
  • caused by the 9 magnitude earthquake that was caused by the build up in strain energy as the pacific plate sub-ducted under the Eurasian plate
  • deaths, injuries,missing people, destroyed buildings
  • repairing the motorway, better and improved warning and monitoring systems where put in place
    -countries sent rescue teams, displacing people
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11
Q

Sumatra tsunami case study

A

-earthquake caused the tsunami
-killed people in 14 different countries,people made homeless,destroyed houses,caused diseases such as cholera
-took months to clean the debris, tsunami early warning systems put in place

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12
Q

Prediction

A

Knowing when and where a natural hazard will strike on a spatial and temporal scale that can be acted on meaningfully

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13
Q

Forecasting

A

Less precise and provides percentage chances of hazards occurring in a particular place

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14
Q

Hazard management cycle

A

It consists of the steps that emergency managers take in planning for and responding to disasters

-preparedness strategies:focus on ensuring that emergency services and people at risk are aware of how to react during an event.Following the event the response section of the hazard cycle is focused on the immediate needs of the population eg such as protection of life and property.This includes emergency medical response,evacuation and transportation,decontamination and the provision of food, water and shelter
-recovery is equivalent to long term responses and is where the city authorities focus on clean up and rebuilding
-mitigation involves authorities looking at the impacts of the hazard and rebuilding in a better way to reduce similar impacts from a future hazard

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15
Q

Park model

A

Stage 1: occurs prior to the event and shows that quality of life is at its normal equilibrium level
Stage 2:where the hazard occurs and again at this point quality of life is normal
Stage 3: where the event has happened and search and rescue is underway. Quality of life drops at this stage and is low for several hours up to servals days depending on the severity of the hazard and the level of development of the country
Stage 4:where relief strategies are underway and there is an organised programme of help. Quality of life improves at this time
Stage 5: refers to long term human response such as rebuilding and restoring normality. Quality of life returns to normal and In some cases can be higher than it was originally

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16
Q

Mitigation

A

Is using technology to remove the cause

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17
Q

Adaptation

A

Working around the effect of a hazard

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18
Q

Modify the loss

A
  • emergency aid
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19
Q

Modify the loss

A
  • emergency aid: long or short then but can make the country dependent
    -insurance:some may rely on insurance to recover losses
20
Q

Modify the vulnerability

A

-hi tech monitoring m: international stateliness and aircraft monitor changes in the earth
-prediction: observing changes in volcanic shapes or low magnitude earthquakes could suggest whether a disaster is likely
- education: teaching communities about hazards and protection enables the community to gain strength and withstand a shock better
-community preparedness:earthquake drills and alarms prepare communities for how to best protect themselves in a disaster

21
Q

Relationship between seismic activity and plate boundaries

A
  • strong relationship
  • earthquakes occur on all plate boundaries
    -most frequent on convergent( destructive and collision) boundaries
    -highest magnitude (>9 on the Ritchter scale ) occur on destructive boundaries
    -significant amount of intraplate activity as a result of :volcanic activity at mantle plumes,faulting in fold mountains, human activity
22
Q

Relationship between volcanic activity and plate boundaries

A

-very strong relationship
-approximately 90% of active volcanoes occur around the pacific ring of fire( largely destructive plate )
-most explosive volcanos(stratovolcanos, composite volcanos) associated with destructive plate boundaries
- shield and fissure volcanos are associated with constructive boundaries

23
Q

Fissure volcano

A

-very liquid lava which is emitted from fractures and flows widespread
-basaltic magma
-effusive eruption(Icelandic or Hawaiian )

24
Q

Shield volcano

A

-large
- sometimes has a collapse caldera
-basaltic magma
- liquid lava emitted from a central vent
-associated with construction plate boundary/mantle plumes

25
Q

Composite volcano

A
  • large
  • more viscous lava
  • destructive plate margin
  • explosive ( pyroclastic debris
    -andesitic magma
  • emitted from a central vent
26
Q

Caldera volcano

A

-destructive plate margin
-opinion eruption
-Associated with plug domes
- andesitic magma
-very large composite volcano collapsed after an explosive period

27
Q

Factors affecting risk

A

-level of vulnerability of a population
-probability of a hazard of a given magnitude occurring

28
Q

Factors affecting vulnerability

A

-level of perceived risk
-social variables within a country eg affluence
-level of economic development
-nature of a hazard: Hazard profile

29
Q

Degg disaster model

A

Shows that in order for a disaster to occur a hazard must interact with a vulnerable population

30
Q

Actual risk

A

The probability of a hazard causing harmful consequences- it is a statistical measurement. Involves the relationship between the vulnerability of a population and the nature of a hazard as shown in the degg model

31
Q

Perceived risk

A

An individuals or groups view of the risk. Affected by things such as awareness:education of hazards and the length of time singe the previous event

32
Q

Vulnerability

A

The susceptibility of a community to a hazard or to the impacts of a hazard event

33
Q

Natural hazard

A

A perceived natural event which has the potential to threaten both life and property

34
Q

Disaster

A

The realisation of a hazard when it causes a significant impact on a vulnerable population

35
Q

Resilience

A

The capacity of a given society to both withstand the impact of a hazard and recover from one

36
Q

Degg disaster model

A

Model which shows that in order for a distaste to occur, a hazard must interact with a vulnerable population

37
Q

Benioff zone

A

An area of seismic activity that corresponds with the slab being thrust downwards in a subduction zone

38
Q

Subduction zone

A

Broad areas where two plates are moving together often with the thinner more dense oceanic plate descending beneath a continental plate

39
Q

Slab pull

A

Where older,colder plates sink at subduction dined because as they cool they become more dense than the underlying mantle

40
Q

Formation of a tsunami

A

Tsunami appears when water is displaced. The main cause is submarine earthquakes however they can be also cause by volcanic activity and landslides. If they are caused by seismic activity vertical movement of crust appears.This displaces the water column above. It produces waves with low amplitude and long wavelengths, radiating outwards.As it reaches the shoreline it produces a vacuum effect sucking all the water away revealing the coastline and the seabed.
The friction causes compression of the waves which then causes them to gain height. The run up is dependent on the topography of the seabed

41
Q

P waves

A

Vibrations caused by compression. Spread quickly at 8km/sec

42
Q

S waves

A

Vibrate at right angles to the directions of travel and cannot travel through liquids
4km/sex

43
Q

L waves

A

Surface waves with vibrations occurring in the horizontal plain. Have high amplitude

44
Q

What does volcanic explositovity measures

A

Volume of ejects
Duration
Height of the column

45
Q

Continental drift -Alfred wegner

A
  • rock type= limestone is formed in warm shallows seas that contain corals- it indicates tropical climates. If found in different places it indicates shift of continents
  • fit of continents: supercontinent called Pangea 175 millions years ago all continents were joined together. No longer the case indicating that continents moved
  • fossils= same type of fossils distributed over different continents. Eg glossopters are distributed across antarica,America, Australia and South America meaning that continents were once joined together
46
Q

Sea floor spreading- Harry Hess

A
  • mid ocean ridges=the invention of sonar allows to obtain a bathymetric profile which allows to revel the high heat flow at mid ocean ridge due to rising magma
    -age of the ocean floor =rocks at the mid ocean ridge are the youngest and they get older as you move away from mid ocean ridge
    -magnetic anomalies =Magnus symmetric about the ridge. Rocks are the same age and have the same polarity so they must have formed together but subsequently have been pushed apart