Tectonic Processes and Hazards Flashcards

1
Q

What was the death toll of the 2011 Tohoku earthquake and tsunami?

A

Over 20,000 people.

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2
Q

Why was the death toll of the 2011 Tohoku earthquake and tsunami so high?

A

40-meter tsunami overwhelmed coastal defenses.

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3
Q

How many people died in the 2010 Haiti earthquake?

A

Around 230,000 people.

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4
Q

Why did the 2010 Haiti earthquake result in such a high death toll?

A

Poorly constructed buildings collapsed easily.

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5
Q

How many relief workers were deployed after the 2008 Sichuan earthquake in China?

A

130,000 people.

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6
Q

Why was the response to the 2008 Sichuan earthquake so large?

A

Magnitude 7.9 required massive aid.

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7
Q

What was the estimated death toll from the 2004 Indian Ocean tsunami?

A

Around 230,000 people.

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8
Q

Why did the 2004 Indian Ocean tsunami cause such widespread destruction?

A

Waves traveled 800 km/h across countries.

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9
Q

How many people died in the 2011 Christchurch earthquake in New Zealand?

A

185 people.

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10
Q

Why was the 2011 Christchurch earthquake so deadly?

A

Shallow depth caused severe shaking.

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11
Q

What was the death toll of the 1995 Kobe earthquake in Japan?

A

6,434 people.

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12
Q

Why did the 1995 Kobe earthquake cause such a high death toll?

A

Magnitude 7.2 caused widespread collapse.

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13
Q

How many people died in the 2010 Mount Merapi eruption in Indonesia?

A

353 people.

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14
Q

Why did the 2010 Mount Merapi eruption cause significant fatalities?

A

Pyroclastic flows moved at 100 km/h.

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15
Q

How many people were evacuated before the 1991 Mount Pinatubo eruption in the Philippines?

A

200,000 people.

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16
Q

Why was the evacuation before the 1991 Mount Pinatubo eruption so successful?

A

Early warning helped avoid casualties.

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17
Q

What was the population affected by the 1995 Montserrat volcanic eruption?

A

Two-thirds of the population evacuated.

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18
Q

Why did two-thirds of Montserrat’s population evacuate during the 1995 volcanic eruption?

A

Intense eruptions prompted large-scale evacuation.

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19
Q

How much seawater was used to cool lava during the 1973 Eldfell eruption in Iceland?

A

6.8 billion litres.

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20
Q

Why was 6.8 billion litres of seawater pumped during the 1973 Eldfell eruption in Iceland?

A

To cool lava and protect infrastructure.

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21
Q

What is the estimated economic loss expected from a future major earthquake in San Francisco?

A

$200 billion.

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22
Q

Why would a future major earthquake in San Francisco result in $200 billion in economic losses?

A

High property values, dense population.

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23
Q

How many countries are covered by the Pacific Tsunami Warning Center (PTWC)?

A

28 countries.

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24
Q

Why does the Pacific Tsunami Warning Center cover 28 countries?

A

Tsunami threats affect many coastal nations.

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25
Q

How many people died in the 2015 Afghanistan earthquake?

A

Around 400 people.

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26
Q

Why was the death toll in the 2015 Afghanistan earthquake relatively low?

A

Sparse population limited fatalities.

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27
Q

How many people died in the 2003 Bam earthquake in Iran?

A

Over 26,000 people.

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28
Q

Why did the 2003 Bam earthquake result in such a high death toll?

A

Collapsing buildings caused mass casualties.

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29
Q

How many people died in the 1999 North Anatolian Fault earthquake in Turkey?

A

Around 17,000 people.

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30
Q

Why was the 1999 North Anatolian Fault earthquake so deadly?

A

Magnitude 7.6 caused widespread destruction.

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31
Q

How many volcanic explosions occur annually at Sakurajima in Japan?

A

Up to 1,000 explosions.

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32
Q

Why does Sakurajima experience up to 1,000 volcanic explosions annually?

A

Continuous volcanic activity, frequent eruptions.

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33
Q

How many people died in the 1991 eruption of Mount Pinatubo in the Philippines?

A

Around 800 people.

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34
Q

Why was the death toll from the 1991 eruption of Mount Pinatubo relatively low?

A

Successful evacuation minimized fatalities.

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35
Q

How many people died in the 1992 Mount Etna eruption in Italy despite the use of lava diversion techniques?

A

Zero casualties.

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36
Q

Why were there no casualties during the 1992 Mount Etna eruption?

A

Lava diversion techniques redirected flows.

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37
Q

What are mega-disasters?

A

Large-scale disasters by areal extent.

38
Q

What else defines mega-disasters?

A

Economic or human impact.

39
Q

How does tectonic setting influence hazards?

A

Affects magnitude, frequency, and type.

40
Q

Where do 90% of tsunamis occur?

A

90% in the Pacific Ocean.

41
Q

How does the Pacific affect vulnerability?

A

Increases regional vulnerability.

42
Q

What is the result of destructive (convergent) margins?

A

More explosive volcanic activity.

43
Q

Why is volcanic activity more explosive at destructive margins?

A

Andesitic lava with higher gas content.

44
Q

What happens at constructive margins?

A

Less explosive basaltic eruptions.

45
Q

How do hotspots affect eruptions?

A

Produce less explosive basaltic eruptions.

Example: Hawaii.

46
Q

Why are island arcs more hazardous?

A

Water-bearing sediments increase volatiles.

47
Q

Give an example of a hazardous island arc.

A

Montserrat.

48
Q

What are the types of volcanic hazards?

A

Lava flows, pyroclastic flows, ash falls.

49
Q

What other volcanic hazards exist?

A

Gas eruptions, lahars, jökulhlaups.

50
Q

What factors are considered in hazard profiles?

A

Magnitude, speed of onset, areal extent.

51
Q

What else is considered in hazard profiles?

A

Duration, frequency, spatial predictability.

52
Q

How do shallow-angle faults affect hazard impact?

A

Affect larger areas, amplify impacts.

53
Q

Give an example of a shallow-angle fault.

A

Afghanistan 2015.

54
Q

What are blind faults?

A

Faults with unpredictable behavior.

55
Q

Give an example of a blind fault.

A

Kobe 1995.

56
Q

How does governance affect vulnerability?

A

Through monitoring, education, mitigation strategies.

57
Q

What does strong governance improve?

A

Disaster response and recovery.

58
Q

What does weak governance reduce?

A

Effectiveness of building codes, planning.

59
Q

What limits governance in some areas?

A

Affordability and budget constraints.

60
Q

Where can weak governance occur?

A

In both developed and developing countries.

61
Q

What is the hazard management cycle?

A

Response, recovery, mitigation, preparedness.

62
Q

Who influences hazard management?

A

Both government and community-led strategies.

63
Q

What limits long-term hazard management?

A

Affordability of measures like aseismic buildings.

64
Q

Can earthquakes be predicted?

A

Earthquakes can be predicted spatially.

65
Q

How are tsunamis detected?

A

After earthquakes, warnings are issued.

Example: PTWC, 2009 Pacific tsunami.

66
Q

What limits prediction accuracy?

A

Extreme events may overwhelm predictions.

Example: Tohoku 2011 tsunami.

67
Q

What do scientists study for earthquake prediction?

A

Stress accumulation on faults.

68
Q

Give an example of a studied fault.

A

North Anatolian Fault.

69
Q

Are volcanic locations well-known?

A

Yes, volcanic locations are generally well-known.

70
Q

How does monitoring equipment help manage volcanoes?

A

Portable equipment improves management potential.

71
Q

What happens if prediction strategies fail?

A

Magnitude may exceed expectations, defenses inadequate.

72
Q

What affects social vulnerability?

A

Population density, isolation, urbanization.

73
Q

What other factors affect vulnerability?

A

Inequality of access to housing. Access to education, healthcare, income.

74
Q

How does high population density affect vulnerability?

A

Amplifies even low-magnitude impacts.

75
Q

How does remoteness affect hazard response?

A

Remote areas are harder to reach.

76
Q

Why are poor communities more vulnerable?

A

Lack of resources to evacuate.

77
Q

How does inequality affect resilience?

A

Influences access to mitigation tools.

78
Q

How does urban infrastructure affect vulnerability?

A

Affects exposure and recovery time.

79
Q

What strategies modify tectonic events?

A

Land-use zoning, hazard-resistant design. Engineering defenses, lava diversion.

80
Q

What strategies modify vulnerability and resilience?

A

Monitoring, prediction, education. Community preparedness.

81
Q

How can loss from disasters be modified?

A

Emergency aid, recovery aid. Insurance, community-led recovery.

82
Q

Which volcanic hazards are manageable?

A

Lava flows (e.g., Eldfell 1973). Lava flows (e.g., Mt. Etna 1992).

83
Q

Which volcanic hazards are hard to manage?

A

Pyroclastic flows, blast waves.

84
Q

What affects the effectiveness of hazard management?

A

Hazard type, frequency, tectonic setting.

85
Q

How does development level affect hazard management?

A

Influences access to mitigation tools.

Example: Zoning, shelters in Japan.

86
Q

How do developed areas compare?

A

They have stronger monitoring systems. Better education and insurance.

87
Q

How does community resilience reduce vulnerability?

A

Better healthcare, housing, and income.

88
Q

How do frequent events improve responses?

A

Areas with frequent events develop better responses.

Example: Merapi as Decade Volcano.

89
Q

How is hazard management effectiveness measured?

A

By death and injury counts. Economic losses, recovery speed.

90
Q

How are high-magnitude events managed?

A

Harder to manage even in developed nations.

Example: Japan 2011.

91
Q

Can smaller events cause major damage?

A

Yes, in vulnerable, unprepared regions.

Example: Haiti 2010.

92
Q

How does development affect hazard management?

A

Affects preparation, response, and reconstruction.