There are many different types of magma, which are all defined by different chemical compositions. It largely depends on the source of the rocks that are being brought to great depth where they are melted and become magmas. For example, magmas in places like Hawaii are very different from magmas in Japan.
And then, as the magma is sitting deep in the earth in a so-called magma chamber, certain minerals will start to crystallise from the magma, and this will make the magma change its composition again.
Finally, the still liquid part of the magma may make it up to earth’s surface, and will cool down very fast – and become a rock.
Think of magma as a mush or semi melted rocks and fully melted rocks. As well as the melted rock that Chris discribes well below, magma also contains suspended large minerals, gas bubbles and dissolved gases.
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