Crust: Solid rock/the crust is solid rock varying in thickness
Oceanic Crust - younger/denser/can be destroyed
Continental Crust - older/lighter/cannot be destroyed
Mantle: Liquid rock (magma)/the mantle in molten rocks
Outer core: Liquid iron and nickel/the outer core is liquid nickel and iron with high pressure and temperature
Inner core: Solid iron and nickel/the inner core is a solid nickel and iron. very high pressure and highest temperature
Plate Boundries
Destructive plate boundries (converging)
Oceanic crust collides with Continental cruset
Oceanic crust is pushed under the Continental crust as it is denser and heavier
The oceanic crust is destroyed in the heat and pressure of the mantle
Builds up heat, pressure and friction and forces the molten rock (magma) UPWARDS
The magma forces its way through the CRUST in a huge and violent volcanic eruption
Volcanoes are formed
Volcanic Island chains are formed
Deep ocean tenches are found where 1 plate is pushed beneath another
Constructive plate boundries (diverging)
Volcanoes are formed
The MID-ATLANTIC RIDGE is a ridge formed beneath the atlantic ocean where 2 plates are splitting apart
Iceland is actually sitting on top of this split and is therefore splitting in to two
A constructive plate boundary is where 2 plates move apart (DIVERGE)
This is caused by convection in the mantle which drag the 2 plates apart
Magma rises to the surface between the two plates and forms a RIDGE under the ocean
Conservative plate boundries
A conservative plate boundary is one where 2 plates push past one another
When one plate catches on another and suddenly jerks past one another, an earthquake is produced
SAN ANDREAS FAULT
Collision plate boundary
A collision boundary is one where 2 continental plates, push together
The two plates, because they are both lighter, continental plates, push upwards against one another. This produces a folding effect on the plates and they form FOLD mountains