Restless Earth
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- Created by: CCauston113
- Created on: 06-05-17 07:17
Structure of the Earth
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Collision boundary
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Destructive boundary
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Constructive boundary
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Conservative boundary
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Shield volcano
Kilauea has been in constant gentle eruption since 1983
Lava is usually basaltic
Made almost entirely of solidified lava, gently sloping sides
Lava flows quickly, and is thin and runny
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Composite volcano
- Example: Mt Pinatubo
- Steep sides, small area, alternate layers of ash and lava
- Viscous lava often 'freezes' in central vent, granitic lava
- Infrequent, unpredictable eruptions
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Volcanoes - causes, impacts and preparation
Causes:
- Hotspots - tectonic plate moves over column of rising magma
- Destructive boundaries - some lightweight materials melt and rise to the surface to form volcanoes
Impacts:
- Kill more with gas and ash than with lava
- Disrupt air travel
- Generate earthquakes and tsunamis
Preparations:
- Evacuation
- Well-trained and funded emergancy services
- Gas emissions, earth tremors and bulging flanks can be used to predict eruptions
- Hazard resistant buildings
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Mount Merapi, India - 2010
Primary Impacts:
Social:
- 360,000 evacuated, some refused to go and others returned during the eruption
- 275 killed by pyroclastic flows
- 570 injured
Economic:
- 2000 farm animals killed
- Villages destroyed, widespread crop damage
- Many flights cancelled
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Mount Merapi, India - 2010
Secondary Impacts:
Social:
- 10km around the volcano declared a danger zone, 2600 unable to return
- Thousands spent weeks living in cramped emergency centres
Economic:
- 1300 hectares of farmland abandoned
- $600 million loss due to severely reduced farming and tourism
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Earthquakes - causes, impacts and preparation
Causes:
- Conservative boundaries - pressure builds up, then sudden release of pressure = earthquake
Impacts:
- People killed as a result of shaking and property destruction
- Lack of shelter and basic supplies
- Fires
Preparation:
- Can't be predicted
- Evacuation routes
- Hazard resistant buildings
- Land use planning
- Disaster kits
- Well-trained and funded emergency services
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Hazard resistant buildings
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LEDC earthquake - Sichuan, China, 2008
Collision boundary
Social Impacts:
- 70,000 died
- 375,000 injured
- 5 million homeless
Economic Impacts:
- Repair of buildings and infrastructure cost £76 billion
- 1 billion unemployed
Responses;
- Prime Minister flew in
- Countries sent aid such as money, medicine, tents and rescue teams
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MEDC earthquake - Kobe, Japan, 2005
Destructive boundary
Port built on reclaimed land that liquified allowing buildings to collapse and sink
Social Impacts:
- 5000 died
- 26,000 injured
Economic Impacts:
- £100 billion damage
Responses:
- Immediate - fire extinguishing, rescue attempts
- Within 8 months - gas, water, electricity, railways and phone lines working again
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Why are some hazards more damaging than others?
Variations:
- Volcanoes are less damaging than earthquakes because people don't live as close
- Some are just more powerful
- Earthquakes vary based on:
- distance from epicentre
- time of day
- preparedness
- quality of emergency services
- LEDCs suffer more socially because:
- higher population density
- less money to spend on preparation and warning systems
- less money to spend on repairs
- MEDCs suffer more economically because:
- people insure property and businesses
- structures cost more
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