Skip to content
Skip to main content

About this free course

Download this course

Share this free course

Practising science: Reading the rocks and ecology
Practising science: Reading the rocks and ecology

Start this free course now. Just create an account and sign in. Enrol and complete the course for a free statement of participation or digital badge if available.

1.3.3 Chemical and mineral composition of igneous rocks

As well as varying in grain size (owing to different cooling rates), igneous rocks also vary in chemical composition and hence in the identity and proportions of minerals present. For instance, the common igneous rock granite contains (as part of the strict geological definition of the term ‘granite’) between 10% and 35% by volume of the mineral quartz (chemical composition silicon dioxide – SiO2). On the other hand, the igneous rock gabbro (Figure 4a) does not usually contain any quartz. This difference is due simply to the fact that granite contains a much higher proportion of the element silicon (Si) than does gabbro. So, chemical composition determines which minerals are present, and cooling rate determines the crystal size of those minerals.

Figure 4
Figure 4 Close-up views of two rocks formed by the cooling of magma of the same chemical composition. (a) Gabbro formed by slow cooling in a subterranean magma chamber. (b) Basalt formed by rapid cooling of magma at the Earth's surface in a lava flow. The field of view is about 2.4 cm across in each case