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Within magma there are volatile gases, predominantly water, but also carbon dioxide, sulphur dioxide etc. At the pressures within a magma chamber these gases are protogases, usually incorporated into the mineral structure in some way i.e. they have the potential to become gases at lower pressures, higher up, when the magma expresses itself as a volcano, where they are released. A magma chamber is not a static repository, but as some minerals created within the magma chamber are heavier (and crystallize at a higher temperature) than others, they sink, and form heavier rocks (e.g. gabbro). The rest of the melt will rise due to being less dense than the surrounding rock, because it is hotter, contains volatiles, and has lost heavier, crystallized minerals; this process continues until the heat is spent, or it emerges as a volcano.

The heat within the magma chamber has the minerals in a heightened state of excitement, therefore they will take up more space, and generally be less dense than their cold equivalents.

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