Locations at Risk from Tectonic Hazards

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Seismic Hazards
Generated when rocks within 700km of the Earth's surface come under such stress that they break and become displaced
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Volcanic Hazards
Associated with eruption events
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Intra-plate Earthquakes
These occur in the middle or interior of tectonic plates and are much rarer than boundary earthquakes
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Volcano
A landform that develops around a weakness in the Earth's crust from which molten magma, volcanic rock and gases are ejected or extruded
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Lithosphere
The surface layer of the Earth is a rigid outer shell composed of the crust and upper mantle. The lithosphere is always moving, slowly, fuelled by rising heat from the mantle which creates convection currents
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Subduction Zones
Two plates are moving together, with the thinner oceanic plate descending beneath a continental plate. Where the plates are locked together, frictional stress builds. When that stress exceeds a given threshold a mega-thrust earthquake occurs
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Locked Fault
A fault that is not slipping because the frictional resistance on the fault is greater than the sheer stress across the fault
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Soil Liquefaction
Water-saturated material can temporarily lose normal strength and behave like a liquid under the pressure of strong shaking
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Intensity
A measure of the ground shaking
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Magnitude
The amount of movement or displacement in the fault which is in turn a measure of energy release
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Epicentre
The location on the Earth's surface that is directly above the earthquake focus
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Other cards in this set

Card 2

Front

Associated with eruption events

Back

Volcanic Hazards

Card 3

Front

These occur in the middle or interior of tectonic plates and are much rarer than boundary earthquakes

Back

Preview of the back of card 3

Card 4

Front

A landform that develops around a weakness in the Earth's crust from which molten magma, volcanic rock and gases are ejected or extruded

Back

Preview of the back of card 4

Card 5

Front

The surface layer of the Earth is a rigid outer shell composed of the crust and upper mantle. The lithosphere is always moving, slowly, fuelled by rising heat from the mantle which creates convection currents

Back

Preview of the back of card 5
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