Hazards 2- Geophysical hazard risk Flashcards

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1
Q

Map of the distribution of volcanoes and earthquakes

A
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2
Q

Describe the distribution of volcanoes

A

-Most volcanoes are found at plate boundaries.

-Some exceptions - Hawaii, which occur over hotspots.

-75% of the Earth’s 550 historically active volcanoes lie along the Pacific Ring of Fire.

-Other areas of active vulcanicity include Iceland, Montserrat and Mt Nyiragongo in the DRC.

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3
Q

At what types of plate boundaries does volcanic activity take place?

A

-At convergent boundaries, where one plate is subducted under another.

-If both plates are oceanic -submarine volcanoes erupt to produce island arcs, like that of the Aleutian Island Arc off Alaska.

-Continental & oceanic plates produces significant volcanic mountain ranges such as the Andes, which forms from the subducting Nazca plate under South America.

-These are the result of high silicate magma rising upwards through the continental crust.

-Volcanoes also form at hotspots and divergent plate boundaries, where shield volcanoes are more common. Eg/ Mauna Loa

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4
Q

At what plate boundaries do earthquakes occur?

A

At all plate boundaries

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5
Q

Map of the distribution of earthquakes

A
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6
Q

What is the ocean fracture zone (OFZ)?

A

A belt of activity through the oceans along the mid-ocean ridges, coming ashore in Africa, the Red sea, the Dead sea rift and California.

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7
Q

What is the continental fracture zone (CFZ)?

A

A belt of activity following the mountain ranges from Spain, via the Alps, to the Middle East, the Himalayas to the East Indies.

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8
Q

Describe the earthquakes at conservative plate boundaries

A

-High frequency, low magnitude earthquakes are more associated with conservative plate boundaries such as the San Andreas Fault in California.

-These earthquakes tend to be shallow in nature and low magnitude but conservative boundaries can also produce much higher magnitude earthquakes but at lower frequency.

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9
Q

Map showing the distribution of landslides

A
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10
Q

Describe the distribution of landslides

A

-Landslides can occur anywhere in the world but there is a higher risk in steep mountainous regions with coarse soil.

-Western regions of the Americas, East Asia and South East Asia stand out as regions of high risk.

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11
Q

What physical and human factors increase the chance of landslides occurring?

A

-Landslide risk is greatest in populated regions with high rainfall events, such as tropical storms and lead to slope saturation and river flooding.

-In addition, regions experiencing population pressure, deforestation, road construction, mining and plantations all lead to greater risk of landslides.

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12
Q

How is earthquake magnitude measured?

A

-Energy release is measured by the logarithmic moment magnitude scale (MMS)

-Damaging effects are measured by the Mercalli scale (measures intensity of shaking)

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13
Q

What is the moment magnitude scale?

A

A logarithmic scale where each level has 10 times the energy of the level below it

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14
Q

Describe 3.0 earthquakes (MM scale)

A

-Minor

-Many a year

-All around the world

-Rarely cause damage

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15
Q

Describe 5.0 earthquakes (MM scale)

A

-Moderate

-Between 1,000 and 1,500 a year

-Damage caused over a small region

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16
Q

Describe 7.0 earthquakes (MM scale)

A

-Major

-Between 10 and 20 a year

-Serious damage over a large area

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17
Q

Describe 9.0 earthquakes (MM scale)

A

-Great

-One every decade (or longer)

-Serious damage over a large region

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18
Q

Describe the IV stage of the Mercalli scale for earthquakes

A

-Shock waves felt indoors

-Windows rattle

-People woken at night

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19
Q

Describe the VII stage of the Mercalli scale for earthquakes

A

-Slight to moderate damage to well-constructed buildings

-Aseismic designs may be slightly damaged

-Walls crack

-People are alarmed

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20
Q

Describe the X stage of the Mercalli scale for earthquakes

A

-Wooden structures and masonry and frame buildings destroyed

-Train rails bent

-Ground may crack

-Landslides caused on steep slopes

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21
Q

Describe the XII stage of the Mercalli scale for earthquakes

A

-Total destruction

-Lines of sight and level distorted

-Objects thrown into the air

-Topography and river courses changed

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22
Q

How is volcano magnitude measured?

A

-Measured by the volcanic explosivity index ( VEI) and based on ejections’ volume, duration, and column height.

-Can be related to the type of plate boundary the volcano is located on.

-Effusive eruptions of basaltic lavas with low VEI ( 0-3) are associated with constructive boundaries or plumes.

-Explosive eruptions with high VEI (4 to 7) of andesitic or rhyolitic lava are associated with destructive boundaries.

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23
Q

What is the VEI scale? (magnitude of volcanoes)

A

A logarithmic scale where each level has 100 times the energy of the level below it

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24
Q

Describe stage 1 of the VEI scale

A

-Small, gentle eruptions

-Less than 10^6 meters of ejected material

-Often small fissure eruptions

-Hawaiian type

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25
Q

Describe stage 3 of the VEI scale

A

-Moderate to large eruptions

-Can be severe

-Up to __ meters of ejected material

-Eruption column of ash up to 10.5 km high

-Eruption phases last up to half a day

-Strombolian type

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26
Q

Describe stage 5 of the VEI scale

A

-Very large eruption

-10^10 meters of ejected material

-Eruption column up to 28km high

-Can be cataclysmic

-Composite volcano type (Plinian or Peleean)

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27
Q

Describe stage 7 of the VEI scale

A

-Very large, colossal eruptions

-10 __ meters of ejected material

-Eruption column height over 47km

-Eruption phases last over half a day

-Composite cone type (ultra-Plinian)

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28
Q

Diagram of the volcanic explosivity index

A
29
Q

What is the tsunami intensivity scale?

A

A logarithmic scale where each level has twice the energy of the level below it

30
Q

Describe the III stage of the tsunami intensivity scale

A

-Run-up height: 2 m

-Floods lowest land

-Small boats carried away

-Some damage to weak buildings

-River flows reversed

31
Q

Describe the IV stage of the tsunami intensivity scale

A

-Run-up height: 4m

-Shore flooded to some depth and land scoured

-Structures damaged

-Larger ships moved inland or out to sea

32
Q

Describe the V stage of the tsunami intensivity scale

A

-Run-up height: 8m

-Widespread flooding

-Major structures damaged

-Soil washed away

-All boats and ships moved inland or out to sea

-Harbors damaged

-Loss of life

33
Q

Describe the VI stage of the tsunami intensivity scale

A

-Run-up height: 16+m

-Complete destruction of some buildings, including some distance from coast

-Coastal lowland and valleys flooded to great depth

-Large ships moved and damaged

-Considerable loss of life

34
Q

Why is understanding recurrence intervals important?

A

It is an important way of measuring risk and preparing for future management of hazards.

35
Q

What are low recurrence intervals often associated with?

A

Relatively poor knowledge and management as well low levels of public perception of risk.

36
Q

What are high recurrence intervals a sign of?

A

Places that experience frequent hazards with high recurrence intervals tend to be better prepared and the public have a lived experience of hazards and so have greater perception of risk.

37
Q

How do geologists use recurrence intervals?

A

-They use these to create detailedseismic hazard curvesthat work on the basis of the probability of an earthquake of a certain magnitude occurring in a certain location.

-From these curveshazard probability mapscan be generated that help authorities plan hazard mitigation and responses both in the short term and long term.

38
Q

What is a hazard?

A

A threat ( natural or human) that has the potential to cause loss of life, injury, property damage, socio-economic disruption, or environmental damage.

39
Q

What is a disaster?

A

A major hazard event that causes widespread disruption to an area and where the affected community is unable to deal adequately without outside help.

40
Q

What is risk?

A

The probability of a hazard event causing harmful consequences ( expected losses in terms of death, injuries, property damage, economy and environment).

41
Q

What is vulnerability?

A

The extent to which a community could be damaged or disrupted by a hazard.

42
Q

What is resilience?

A

The ability or capacity of a community to withstands the effects of a natural hazard & bounce back ( adaptation, recovery).

43
Q

What is the disaster risk equation?

A
44
Q

When does the risk of a disaster increase?

A

As the frequency or severity of hazards increases, people’s vulnerability increases and people’s capacity to cope (ability to cope with the consequences) is decreased.

45
Q

Picture of the Pressure and Release (PAR) model

A
46
Q

Why do people live in hazardous areas?

A

-Fatalist approach – ‘God’s will’, no alternative, losses accepted, Russian roulette – optimistic approach.

-Acceptance approach – accept the risk, because economic advantages are greater.
e.g. Tourism, energy, minerals, agriculture.

-Adaptation approach – Events can be prevented & early warnings given. The area has been made safer by technology, fewer people will be affected.

47
Q

How does gender impact a person’s vulnerability to hazards?

A

-Women are more homebound than men, so when hazards strike, they are often the victims of collapsing buildings.

-During tsunamis, women have been impacted more because of their caring roles toward children and the elderly.

-They get caught up in their attempt to help family members whilst men are at work, are independent and so more able to make survival decisions.

-Oxfam survey - four times as many women as men were killed during the 2004 tsunami -men taught how to swim and climb trees at young ages, while women were not.

-After the Haiti earthquake women were more vulnerable with rape on the rise.

48
Q

What type of boundary did the Haiti earthquake occur at?

A

Conservative (transform) boundary

49
Q

When was the Haiti earthquake?

A
50
Q

Describe the geography of the Haiti earthquake

A

-Epicenter was close to capital Port au Prince ( 25km away)

-Focus shallow – only 13km

-Spatial extent was quite large at 120km2,

-Hadn’t experienced an earthquake in 150yrs, so no experience,

-Magnitude 7

-Speed of onset was sudden ( 30-60 seconds).

51
Q

Living conditions in Haiti at the time of the earthquake

A

-Buildings & infrastructure were not earthquake-proof

-High unemployment

-People relied on informal sector

-Many lived in slums

-72% lived in poverty

-Homes built on slopes.

52
Q

What pressures did Haiti face (clarify whether this is before or after the earthquake)

A

-Rapid rural to urban migration, growth of slums..all put pressure on local authorities.

-Hillsides stripped of trees to make more space.

-Low HDI.

-Education levels are lower, so perception & risk low.

53
Q

How was poor governance a cause of the Haiti earthquake (reword)

A

-Basic needs were not being met – limited access to roads, electricity & sanitation.

-Poor planning – deforestation & building on hillsides, no preparedness, didn’t ensure correct building codes, corrupt government.

-Access to health care & education is poor.

-Low-income groups lack a ‘safety net’ after a disaster – personal one ( savings, food) or government one ( social security, aid, free healthcare)

54
Q

How does population density affect how at risk a place is to a hazard?

A

Highly-populated areas may be hard to evacuate

55
Q

How do isolation and poor accessibility affect how at risk a place is to a hazard?

A

This can slow rescue and relief

56
Q

How does a place’s degree of urbanization affect how at risk it is to a hazard?

A

-Death tolls can be high in urban areas because of the concentration of at-risk people

-Urban areas usually have more assets (hospitals, food stores, and transport systems) than rural areas, which increases resilience.

-L’Aquila, Italy is 60km away from Rome, and the Civil Defence was able to make a rapid response.

57
Q

How does timing affect how at risk a place is to a hazard?

A

-The L’Aquila 6.3 magnitude (Italy) earthquake in 2009 killed 308 & injured 1,500.

-It hit at 3:32 am so people had no chance to make quick decisions.

-However, if it had occurred during the school day, 100s if not 1,000s could have been killed due to poor school infrastructure.

58
Q

Describe the Sulaweshi (Indonesia) earthquake

A

-7.5 mag earthquake in 2018

-2nd Hazards – tsuanami

-Town of Donnaggala is located on the low coastal plain and felt the full force of the waves.

-The town of Palu suffered from liquefaction and as it was located at the end of a coastal inlet, suffered the largest waves, as they were funneled, gaining in height.

-Part of the town ended up flowing on town hill due to liquefaction.

59
Q

Describe the Nepal earthquake

A

-7.9 earthquake, April 2015

-2nd hazards – caused an avalanche at Everest Base camp

-District of Rasuwa – hospital located at

-2,030m devastated – couldn’t use roads due to fears of landslides, had to shuttle supplies in on helicopters.

60
Q

Describe the Greenland earthquake

A

-Landslide in a fjord in Nugaatsiaq led to a 90m tsunami, with 3 villages having to be evacuated.

-The capital Nuuk is 3,000km away – ltd roads, and resources 7 difficult to access by boat made the response challenging.

61
Q

What factors influence vulnerability to hazards and resilience?

A

-Unequal access to education

-Unequal access to housing

-Unequal access to healthcare

-Urbanization

-Unequal access to income opportunities

-Population density

-Governance (a synoptic theme)

-Accessibility

62
Q

How does unequal access to education influence vulnerability and resilience?

A

-Some people lack formal education, so don’t know about tectonic processes and hazards or what actions to take.

-These people are also unable to participate in decision-making and planning.

-Traditional knowledge may also get lost (for example, Turkey: decline in seismic building methods due to rural-urban migration)

63
Q

How does unequal access to housing influence vulnerability and resilience?

A

-Some people are poor and lack resources, so they do not live in strong buildings that can withstand hazards (for example, Bam, Iran (2003): 31,000 killed when unbaked clay houses collapsed).

-Better housing belonging to richer people may be exposed on a coast (tsunami) or steep slopes (landslides) (e.g. California).

64
Q

How does unequal access to health care influence vulnerability and resilience?

A

-Poorer people, especially those in developing countries, may lack access to doctors and medicines.

-During a hazard, people need medical care for injuries, and afterward to stop diseases from spreading.

-Medical aid is not always fairly distributed (for example, in Gujarat, India (2001), ethnic minority groups did not get their fair share of healthcare after the earthquake).

65
Q

How does unequal access to income opportunities influence vulnerability and resilience?

A

-Those formally employed have a regular wage but those working in the informal sector (common in developing countries) or unemployed do not.

-This affects their ability to save for safety improvements, insurance, stockpile emergency resources, or get essentials after a hazard.

-Poorer people may have to live in risky areas (for example, farmers around Mount Merapi (2010) returned to their livestock within the volcanic eruption evacuation zone).

66
Q

How does urbanization influence vulnerability and resilience?

A

-Around the world, urban areas are growing.

-This increases risk where buildings are not seismic, and considerable destruction is possible (for example, cities in developing countries like Haiti (Port-au-Prince) are more at risk than developed countries like Japan (Tokyo).

-Even in prepared cities, insurance costs may be high (for example, Taipei has an estimated $181 billion of risk 2015-25)).

67
Q

How does population density influence vulnerability and resilience?

A

-The denser the population, the larger the number of people that can be affected by a tectonic hazard (for example, Japan and Indonesia).

-More people are being affected by hazards over time, due to population growth and rural-urban migration, especially in emerging and developing countries.

68
Q

How does governance (a synoptic theme) influence vulnerability and resilience?

A

-Corruption in local or national governments prevents investment in hazard mitigation and adaptation such as stronger housing or disaster preparedness such as warning systems, education, and health care.

-Help and information agencies may not get set up and investment in, and use of, technology may not happen.

-Developing and emerging countries may rely on international links to get aid.

-In these countries, weak government regulations r enforcement may mean preparation for hazards are low (e.g. building codes).

69
Q

How does accessibility influence vulnerability and resilience?

A

-Some countries or regions are isolated by distance or physical barriers such as mountains or the sea.

-This can cause problems after a hazard (e.g. Kashmir, India, 2005) as aid is difficult to deliver.

-Vanuatu is a high-risk country because it is a nation of many islands (with no mobile phone service) spread over a large area of the Pacific Ocean, so people may have no options of moving to safer locations.