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Hazards - Coggle Diagram
Hazards
Tectonic Hazards
Convection currents
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This creates a current as rock is heated and cools, this is how the crusty plates move
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Pangea
All continents used to be part of one big landmass, proven because they all fit together and the same fossils in one continent were found in another (they would have been right next to eachother)
Plate margins
Constructive/divergent
Two tectonic plates are moving apart and magma is rising through the gap which creates shield volcanoes like on Iceland.
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Destructive/convergent
A continental and an oceanic plate margin are moving towards each other, the oceanic plate which is more dense and thinner subducts under the continental plate
The subduction creates a lot of friction, pressure and tension which causes earthquakes to happen
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The subducting plate becomes magma as it melts in the 1500 degrees C heat of the mantle. This magma is forced up into a magma chamber of a volcano and causes volcanic eruptions.
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Conservative
Plates move in same direction or opposite direction, not towards or away from eachother
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Case studies
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HIC Hazard: Japan 2011
Primary Impacts
Tsunami
500 mph in parts, highest at 38m
18,000 deaths, most drowning because of the tsunami
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Secondary Impacts
Loss of business, trade, export, income e.g. Toyota
500,000 people homeless, mostly due to nuclear fallout from Fukushima Daiichi - reactor couldn't be cooled because backup generators for coolant were damaged by the strong waves.
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Caused because Japan is on a destructive plate boundary, oceanic plate subducting under the continental plate
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Responses
There was a 60 second alert because of automatic responses from seismometers around the country and out at sea
Emergency services scrambled to help people, fire engines, ambulance, rescue helicopters.
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