Classification
Stones branch like a family tree. Minerals are grouped by the Nickel-Strunz system, rocks by how they form.
Minerals
71Naturally formed solids with a definite chemical composition and an ordered atomic arrangement (crystal structure). The International Mineralogical Association (IMA) recognises more than 6,000 mineral species today.
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Elements
6Minerals made of a single element: gold, copper, sulfur, diamond…
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Sulfides and sulfosalts
6Compounds of metals with sulfur; the main ores of many metals.
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Halides
2Minerals built with chlorine, fluorine and similar elements: rock salt, fluorite.
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Oxides and hydroxides
19Compounds of metals with oxygen: corundum, hematite, quartz (in Nickel-Strunz).
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Carbonates and nitrates
4Calcite, dolomite, malachite… Many fizz in dilute acid.
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Borates
3Boron minerals. The world’s largest boron deposits are in Türkiye.
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Sulfates
3Gypsum, baryte, celestine…
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Phosphates
2Apatite, turquoise… Our teeth and bones are made of an apatite-like material.
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Silicates
26Built from silicon–oxygen tetrahedra, the largest class, making up most of Earth’s crust.
Nesosilicates
6Isolated tetrahedra: olivine, garnet, zircon, topaz.
Sorosilicates
3Paired tetrahedra: epidote, zoisite (tanzanite).
Cyclosilicates
4Rings: beryl (emerald), tourmaline.
Inosilicates
3Chains: pyroxenes, amphiboles, jade.
Phyllosilicates
6Sheets: micas, talc, clay minerals, meerschaum.
Tectosilicates
4Frameworks: feldspars, zeolites.
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Organic compounds
0Rare minerals of organic origin.
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Rocks
29Natural aggregates of one or more minerals (sometimes glass or organic matter). Rocks are divided into three great groups by how they form.
Igneous rocks
12Formed when molten rock (magma or lava) cools and solidifies.
Sedimentary rocks
9Formed from accumulated and hardened fragments, chemical precipitates or the remains of living things.
Clastic
5From fragments such as sand, gravel and clay: sandstone, conglomerate.
Chemical and biochemical
3Precipitated from water or built from shells: limestone, travertine, rock salt.
Organic
1From plant remains: coal.
Metamorphic rocks
8Formed when existing rocks are transformed by heat and pressure without melting.
Foliated
3Minerals aligned in layers: slate, schist, gneiss.
Non-foliated
5Massive, without layering: marble, quartzite.
Mineraloids
3Natural substances that resemble minerals but lack an ordered crystal structure: opal, volcanic glass.
Organic gems
4Stones produced by living things or formed from their remains: amber, pearl, coral, jet (Oltu stone).
Meteorites and impact stones
4Stones and masses of metal that fell to Earth from space, and the glasses that large impacts created on Earth.
Stony meteorites
1Made mostly of silicate minerals; most meteorites that fall belong here.
Iron meteorites
1Made of iron–nickel alloy; pieces of the cores of shattered planetesimals.
Stony-iron meteorites
1Roughly equal mixtures of metal and silicate; pallasites belong here.
Impact glasses
1Not meteorites: formed from Earth rocks melted and flung out by large impacts (tektites).