Tectonic Hazards Flashcards
Conservative Plate Margin
Tectonic plate margin where two tectonic plates slide past each other.
Constructive Plate Margin
Tectonic plate margin where rising magma adds new material to plates that are diverging or moving apart.
Destructive Plate Margin
Tectonic plate margin where two plates are converging or coming together and the oceanic plate is subducted. It can be associated with violent earthquakes and explosive volcanoes.
Earthquake
A sudden or violent movement within the Earth’s crust followed by a series of shocks.
Immediate Responses
The reaction of people as the disaster happens and in the immediate aftermath.
Long-term Responses
Later reactions that occur in the weeks, months and years after the event.
Monitoring
Recording physical changes, such as earth tremors around a volcano, to help forecast when and where a natural hazard might strike.
Plate Margin
The margin or boundary between two tectonic plates.
Planning
Actions taken to enable communities to respond to, and recover from, natural disasters, through measures such as emergency evacuation plans, information management, communications and warning systems.
Prediction
Attempts to forecast when and where a natural hazard will strike, based on current knowledge. This can be done to some extent for volcanic eruptions (and tropical storms), but less reliable for earthquakes.
Primary Effects
The initial impact of a natural event on people and property, caused directly by it, for instance the ground buildings collapsing following an earthquake.
Protection
Actions taken before a hazard strikes to reduce its impact, such as educating people or improving building design.
Secondary effects
The after effects that occur as indirect impacts of a natural event, sometimes on a longer timescale, for instance fires due to ruptured gas mains resulting from the ground shaking.
Tectonic Hazard
A natural hazard caused by movement of tectonic plates (including volcanoes and earthquakes).
Tectonic Plate
A rigid segment of the Earth’s crust which can ‘float’ across the heavier, semi-molten rock below. Continental plates are less dense, but thicker than oceanic plates.
