Skip to main content

Classification of minerals

Short answer

Minerals are classified by abundance (rock-forming, accessory, ore), chemically (native elements, sulphides, oxides, silicates, etc.), and by colour (felsic light, mafic dark). Silicates are the largest group, about 90% of the crust.

How do you classify minerals?

Minerals are classified in several ways.

1. Based on abundance and role in rocks

  • Rock-forming minerals: abundant, form the bulk of rocks (quartz, feldspar, mica, amphibole, pyroxene, olivine, calcite).
  • Accessory minerals: occur in small amounts (zircon, apatite, magnetite).
  • Ore minerals: contain metals of economic value (galena, hematite, chalcopyrite).

2. Chemical classification (most common)

  • Native elements (gold, graphite), sulphides (pyrite), oxides (hematite), halides (halite), carbonates (calcite), sulphates (gypsum), phosphates (apatite) and silicates (the largest group, about 90% of the crust).

3. Colour-based

  • Felsic (light-coloured: quartz, feldspar) and mafic (dark: pyroxene, olivine, biotite).

✓ Answer checked by Claude Opus 5.5 (high effort)

All Engineering Geology I chapter 3 questions →