The crust is 'cracked' into huge pieces called tectonic plates. Oceanic plates lie beneath the oceans and continental plates form the continents. The tectonic plates are less dense than the mantle and float on top of it.
Convection Currents in the mantle transfer energy to the plates, causing them to move very slowly.
In a volcano the magma is forces out onto the surface of the Earth as a stream of lava.
The lava cools quickly to form igneous rock with small crystals.
When magma is forced up through cracks in the crust but does not reach as far as the surface, it cools more slowly. This forms igneous rocks with large crystals.
Iron rich magma, which is runny and gives lava that runs slowly from the volcano, forms basalt. Silica-rich magma, which gives lava that is ejected explosively, forms rhyolite.
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