Tectonics Pack I Flashcards

(20 cards)

1
Q

What indicators change before an earthquake?

A
  • Height of water table
  • Levels of radon gas dissolved in water (increases)
  • Earth’s magnetic field
  • Animal behaviour
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2
Q

How can earthquakes be monitored?

A
  • Small movements along fault: laser reflector, creep meter, gravity meter, tilt meter
  • Changes in rock stress: strain meter
  • Groundwater movements and water table heights: well levels and groundwater measurements
  • Radon gas: radon gas meter
  • Changes in Earth’s magnetic field: magnetometer
  • Smaller foreshocks: seismograph and seismometer
  • Animal behaviour
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3
Q

Why can’t earthquakes be predicted?

A
  • Date, time, location and magnitude cannot all be predicted yet (USGS standards)
  • Unofficial predicts occur when something happens that is thought to be a precursor to a major quake
  • But often these activities happen without an earthquake
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4
Q

How can tsunamis be predicted and monitored?

A
  • By monitoring undersea seismic activity
  • Tide gauges, tsunami detection buoys and pressure recorders detect changes that show a tsunami has been generated
  • Therefore, areas can be warned of its arrival
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5
Q

What is the Indian Ocean Tsunami Warning System (IOTWS)?

A
  • Fully operational in 2011
  • Covers 28 countries and 2 billion people
  • UNESCO and India were key players
  • Cost $150-200 million
  • Can predict risk to coastal areas, height of wave and vulnerable buildings
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6
Q

What environmental changes happen before a VE?

A
  • Seismic activity
  • Ground deformation
  • Gas emissions
  • Thermal changes
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7
Q

How is seismic activity before a VE monitored?

A
  • Seismometers and seismographs
  • Distributed acoustic sensing
  • May show an increase in activity over time
  • Suggests rising magma fracturing rocks
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8
Q

How is ground deformation before a VE monitored?

A
  • Tilt meters and laser measures
  • Detect tiny changes in slope angle and the distance between points
  • Suggests rising magma is displacing ground above
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9
Q

How are gas emissions before a VE monitored?

A
  • Ground-based, airborne and satellite detectors
  • Measures changes in the amount and composition of gas emissions
  • Gases passing through lakes can be detected by changes in colour and acidity
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10
Q

How are thermal changes before a VE monitored?

A
  • Detectors and satellites
  • Register changes in surface and lake temperature
  • Suggests increase in activity
  • Visible signs are increasing discharge from hot springs and death of vegetation
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11
Q

How can lahars be monitored?

A
  • Observations with remote video cams and drones
  • Seismometers recording active lahar vibrations
  • Allow short term warnings
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12
Q

What are the 3 ways to mitigate the hazard?

A
  • Modify the event
  • Modify the loss
  • Modify vulnerability
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13
Q

How can a VE event be modified?

A
  • Control flow of lava
  • By spraying sea water on advancing lava so it cools (e.g. Iceland 1973)
  • With barriers to divert lava flows away from populated areas (e.g. Mt Etna 1991)
  • These methods only worked because the eruption had stopped
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14
Q

How can human vulnerability to a VE be modified?

A
  • Monitoring and predication
  • Warning systems
  • Evacuation plans
  • Hazard mapping (e.g. lahar or lava flow risks to influence planning and zoning)
  • Education to help people learn how to prepare
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15
Q

How can an earthquake event be modified?

A

Not possible to yet

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16
Q

How can human vulnerability to an earthquake be modified?

A
  • Building codes requiring aseismic buildings (e.g. Japan)
  • Education and earthquake drills
  • Hazard mapping (e.g. liquefaction prone areas to prevent building)
  • Use of smart technology
17
Q

What are the limitations of aseismic building codes?

A
  • Difficult to retrofit to old buildings
  • Costs are too high for most buildings
  • Difficult to enforce codes in LICs due to lack of political will and money
18
Q

How can human vulnerability to a tsunami be modified?

A
  • Warning and prediction systems
  • Education
  • Clearly marked evacuation routs
  • Coastal zone management and land use planning (e.g. set back zones with no development)
19
Q

How can a tsunami event be modified?

A
  • Coastal defences and hard engineering (e.g. Japan’s 400km chain of 12-15m sea walls)
  • Soft engineering (e.g. restoring mangroves to dissipate wave energy)
20
Q

How can the loss to a VE, earthquake or tsunami be modified?

A
  • Rescue and relief efforts
  • Aid from governments and NGOs to provide food, clean water and shelter
  • Insurance but mainly available in HICs and might not cover
  • Individual responses (e.g. purchasing emergency survival kits)