Igneous rocks are primarily classified based on their texture and composition. Here are the major types:
1. Granite
- Composition: Felsic, primarily composed of quartz, feldspar (usually orthoclase and plagioclase), and mica.
- Texture: Coarse-grained (phaneritic), meaning the individual mineral crystals are large enough to be seen with the naked eye. Typically has a light color.
2. Rhyolite
- Composition: Felsic, similar to granite but with a higher proportion of volcanic glass and usually contains quartz and feldspar.
- Texture: Fine-grained (aphanitic), where crystals are too small to see without a microscope. Often has a lighter color and may show flow banding.
3. Diorite
- Composition: Intermediate, composed of plagioclase feldspar, hornblende, and sometimes quartz or biotite.
- Texture: Coarse-grained (phaneritic) with a salt-and-pepper appearance due to the contrasting colors of the minerals.
4. Andesite
- Composition: Intermediate, primarily made up of plagioclase feldspar with some biotite, hornblende, or pyroxene.
- Texture: Fine-grained (aphanitic) or porphyritic, containing larger crystals (phenocrysts) in a finer-grained matrix.
5. Basalt
- Composition: Mafic, predominantly composed of pyroxene, olivine, and plagioclase feldspar.
- Texture: Fine-grained (aphanitic) with a dark color. Some basalts may exhibit a vesicular texture, containing small gas bubbles.
6. Gabbro
- Composition: Mafic, composed mainly of plagioclase feldspar, pyroxene, and sometimes olivine.
- Texture: Coarse-grained (phaneritic) with a dark color, similar mineral composition to basalt, but with larger crystals.
7. Pumice
- Composition: Felsic to intermediate, usually formed from volcanic glass with a high gas content.
- Texture: Light-colored, very porous, and glassy. It can float on water due to its low density.
8. Obsidian
- Composition: Felsic, composed mainly of silica.
- Texture: Volcanic glass, usually glassy and very smooth, lacking a crystalline structure.
9. Scoria
- Composition: Mafic, composed mainly of basaltic material.
- Texture: Vesicular, with numerous gas bubbles, giving it a light weight and reddish-brown to black color.
These major types highlight the diversity in igneous rock formation processes, mineral compositions, and textural characteristics.