Classification & nomenclature

How scientists name rocks and minerals—what a name implies about composition, texture, and origin.

Core ideas

How names work

Rock names are shorthand. They often encode mineral proportions, grain size, and formation setting.

Mineral names

A mineral species is defined by composition + crystal structure (e.g., quartz = SiO₂). Variants may be described by habit, color, or impurities.


Rock names

Rocks are classified by origin (igneous/sedimentary/metamorphic) and then refined by composition and texture (e.g., basalt vs. gabbro).


Modifiers

Terms like “porphyritic,” “vesicular,” “micaceous,” or “calcareous” add detail without changing the base name.


Formal systems

Igneous: QAPF/TAS; sedimentary: siliciclastic vs. carbonate; metamorphic: protolith + grade + fabric.

Examples in images

Textures and structures that commonly appear as modifiers in scientific names.

Granite texture showing interlocking crystals Sedimentary bedding layers Metamorphic foliation in schist outcrop Basalt column texture
Granite texture showing interlocking crystals Sedimentary bedding layers Metamorphic foliation in schist outcrop Basalt column texture
Granite texture showing interlocking crystals Sedimentary bedding layers Metamorphic foliation in schist outcrop Basalt column texture
Granite texture showing interlocking crystals Sedimentary bedding layers Metamorphic foliation in schist outcrop Basalt column texture
Granite texture showing interlocking crystals Sedimentary bedding layers Metamorphic foliation in schist outcrop Basalt column texture
Granite texture showing interlocking crystals Sedimentary bedding layers Metamorphic foliation in schist outcrop Basalt column texture

Continue with the overview

Return to the Stone Science overview for the full chapter list and glossary.