Crust: The outer layer of the earth
Plate: A section of the earth's crust
Plate margin: The boundary where two plates meet
Mantle: The dense mostly solid layer of the earth between the outer core and the crust.
Convection currents: The circular currents of heat in the mantle
Destructive: A plate margin where two plates are moving towards each other, resulting in one plate sinking beneath the other.
Constructive: Two plates that are moving apart
Conservative: Two plates sliding alongside each other
Earthquake: A sudden, often violent shift in the rocks forming the earth's crust, which is felt at the surface
Volcano: An opening in the earth's crust through which molten lava, ash and gases are ejected.
Oceanic crust: A tectonic plate made of dense iron rich rock that forms the ocean floor.
Continental crust: A tectonic plate made of low density continental rock that will not sink under another plate.
Subduction: When oceanic crust sinks under continental crust at a destructive margin
Collision: When two plates of continental crust meet 'head on' and 'buckle'.
Past exam questions:
Explain how volcanoes from at destructive plate margins
- Convection currents in the lower mantle cause the plates to move towards each other
- If plates are continental v oceanic crust, the oceanic (denser) crust will sink below the continental (lighter) crust in a process called subduction.
- Great pressure is exerted and heat is produced from friction between the plates which destroys (melts) the oceanic plate to form magma.
- The magma is lighter than its surroundings so rises to the surface causing violent volcanic eruptions.
Explain how earthquakes occur at conservative plate margins
- Plates moving in similar directions (but not the same)
- The pressure builds up as the plates stick
- Sudden release causing the jerking movement which is the earthquake
- For example the San Andreas Fault
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