Restless Earth

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  • Created by: mieke.r
  • Created on: 02-04-17 07:20
Asthenosphere
part of the Earth's mantle. It is a hot, semi-molten layer that lies beneath the tectonic plates. It is between 20 and 70 km thick
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Collision Plate Boundary
where two plates collide
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Conservative Plate Boundary
formed when two plates slide past each other
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Constructive Plate Boundary
formed when two plates move apart
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Continental Crust
the part of the earth's crust that makes the continents; it is between 20 and 100km thick
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Convection Currents
transfer heat from one part of a liquid or gas to another. In the earth's mantle, the currents which rise from the earth's core are strong enough to move the tectonic plates on the earth's surface
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Destructive Plate Boundaries
boundary where two plates are pushed together
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Evacuation
when people move from a place of danger to a safer place
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Long-term Planning
training in health care
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Magnitude
of an earthquake, an expression of the total energy released
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Oceanic Crust
the part of the earth's crust which is under the oceans; it's made of basalt and is between 5km and 10km thick
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Plate Boundaries
where tectonic plates meet
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Prediction
saying that something will happen in the future. A scientific prediction is based on statical evidence
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Preparation
Shock absorbers in buildings, earthquake proofing hazardous zones
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Short- term Emergency relief
food given in emergency
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Tectonic Hazard
are natural events that affect people and property
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Lithosphere
the uppermost layer of the earth, it is cool and brittle. It includes the very top of the mantle and the crust
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Magnetosphere
a force field that protects the earth from harmful radiation from space and the sun
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Plumes
bring magma to the surface. If magma breaks through the crust the lava erupts from a volcano
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Subduction
describes the oceanic crust sinking into the mantle at a destructive plate boundary
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Volcanic Explosivity Index
measures destructive power on a scale from 1 to 8
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Primary Effects
caused instantly by the eruption. These are directly linked to the volcano
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Secondary Effects
in the hours, days or weeks after the eruption. These are often caused by the volcano
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Social impacts
The impacts on people
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Economic Impacts
the impacts on the wealth of the area
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Refugees
people who are forced to move due to a natural hazard or war
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Aid
help, It can be short term such as food given in emergency, or long term, such as training in health care
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Relief Effort
like aid. It is help given by organisations or countries to help those who are facing emergency
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Aftershocks
often occur as the fault 'settles' into its new position. They can injure or kill rescuers
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Radioactive Decay
some elements are naturally unstable and radioactive. Atoms of these elements release particles from their nuclei and give off heat
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Seismometer
a machine for recording and measuring an earthquake
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Other cards in this set

Card 2

Front

where two plates collide

Back

Collision Plate Boundary

Card 3

Front

formed when two plates slide past each other

Back

Preview of the back of card 3

Card 4

Front

formed when two plates move apart

Back

Preview of the back of card 4

Card 5

Front

the part of the earth's crust that makes the continents; it is between 20 and 100km thick

Back

Preview of the back of card 5
View more cards

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