Classifying Igneous Rocks
Magma Compositions - Igneous rocks are often classified by mineral (chemical) composition.
- Ultramafic
- Rare, high in magnesium and iron. Magmas with this composition are composed entirely of ferromagnesian silicates like olivine and pyroxenes.
- Rare, high in magnesium and iron. Magmas with this composition are composed entirely of ferromagnesian silicates like olivine and pyroxenes.
- Mafic (or basaltic)
- Mafic: magnesium and ferrum (iron). Contains substantial dark silicate minerals like olivine and pyroxenes, and calcium-rich plagioclase feldspar.
Extrusive / Volcanic Rock: Basalt
Intrusive / Plutonic Rock: Gabbro
- Aphanitic texture
- Composed mainly of pyroxene and calcium-rich plagioclase
- Most common extrusive igneous rock
- Phaneritic texture
- Composed of pyroxene and calcium-rich plagioclase
- Comprises most of the oceanic crust
- Mafic: magnesium and ferrum (iron). Contains substantial dark silicate minerals like olivine and pyroxenes, and calcium-rich plagioclase feldspar.
- Intermediate (or andesitic)
- Contains at least 25% dark silicate minerals. Associated with explosive volcanic activity
Extrusive / Volcanic Rock: Andesite
Intrusive / Plutonic Rock: Diorite
- Aphanitic texture
- Dark grey color
- May have plagioclase phenocrysts
- Phaneritic texture
- Composed of plagioclase & hornblende
- Black and white make DIORITE
- Contains at least 25% dark silicate minerals. Associated with explosive volcanic activity
- Felsic (or granitic)
- Felsic: feldspar and silica. Composed almost entirely of light-colored silicates
Extrusive / Volcanic Rock: Rhyolite
Intrusive / Plutonic Rock: Granite
- Aphanitic texture
- Buff or pink color
- May have glass phenocrysts
- Phaneritic texture
- >25 % quartz, about +65 % feldspar
- The term covers a wide range of rocks (Often incorrectly)
- Felsic: feldspar and silica. Composed almost entirely of light-colored silicates
- Varied Compositions
- Obsidian
- Glassy texture
- Dark in color
- Pumice
- Glassy texture
- Light in color
- Frothy appearance with numerous voids due to escaping gases
- Pyroclastic rocks
- Composed of fragments ejected during a volcanic eruption
- Tuff – ash-sized fragments
- Volcanic breccia – particles larger than ash
- Obsidian
Common Minerals Found In Igneous Rocks
Olivine | = | olive green |
Pyroxene (Augite) | = | dark green |
Amphibole (Hornblende) | = | black |
Biotite | = | black |
Plagioclase | = | white / grey |
Potassium Feldspar | = | pink / salmon |
Muscovite | = | silvery |
Quartz | = | clear |
Tourmaline* | = | black |
Magnetite* | = | black |