GCSE Tectonics 1

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Created by:

rgamesby  on August 5, 2009

Subjects:

plate tectonics

Description:

A set to help you revise the Restless Earth topic

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GCSE Tectonics 1

Subduction
Where one plate is pushed underneath another plate
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Subduction Where one plate is pushed underneath another plate
Destructive plate margin Where one plate sinks under another, destroying the old crust
Constructive Plate margin Where the two plates move apart making new crust
Conservative plate margin Where one plate slides past the other sideways
Crust the outer layer of the Earth
Mantle the layer of the earth between the crust and the core
Convection current the movement of magma in the mantle caused by heating of the material
Inner Core a dense sphere of solid iron and nickel at the center of Earth
Plate Margin Where the two plates meet
Continental crust granitic part of the Earth's crust that makes up the continents. Continental crust is also called sial because it consists largely of silica and aluminum and averages about 40km thick
Oceanic crust thin, more dense than continental crust, subducting crust
Fold mountains these are mountains formed as the plates move together and folds are formed as the the layers are squeezed horizontally.
Ocean Trench deep valley in the ocean floor that forms along a subduction zone
Ocean ridge created at a divergent boundary where the ocean plates spread apart. Magma rises out to form underwater mountains.
Composite volcano tall, cone-shaped volcano in which layers of lava alternate with layers of ash
Shield Volcano a wide gentle sloping volcano made of layers of lava and formed by quiet eruptions.
Pacific ring of fire Zone of crustal instability, volcanism, and earthquakes in the Pacific region.

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