What’s in nature?
From elements to living things: what sits inside what in nature, and what comes from what? Tap the mineral, rock and other stone branches to open each stone’s path.
The base: elements
The building blocks of everything, living or not. 118 elements are known today; 94 occur in nature and 24 were made in the laboratory.
The three kinds of element (these are not below the elements; they are the elements):
Found pure in nature and counted as stones: Gold, Silver, Copper, Platinum, Bismuth, Sulfur, Diamond and Graphite (both pure carbon).
When elements combine, they form compounds (water, salt, quartz) and mixtures (air, soil, petroleum). About 99% of the human body is six elements: oxygen, carbon, hydrogen, nitrogen, calcium and phosphorus.
Solid, liquid and gas are states, not kinds: the same water becomes ice (a mineral) when it freezes and vapour when it is heated.
The idea of “four elements” goes back to Empedocles around 450 BC and was abandoned in the late 1700s. Science today does not count them as elements:
- Water is a compound: hydrogen + oxygen (H₂O).
- Air is a mixture: 78% nitrogen, 21% oxygen, 0.9% argon…
- Soil is a mixture: minerals, organic matter, water and air.
- Fire is not a substance but a reaction: fuel burning rapidly with oxygen, giving off heat and light.
Living things
Cellular life falls into three great groups (“domains”). The system was proposed by Carl Woese and colleagues in 1990.
The mushroom we eat is only the “fruiting body” of a fungus that lives underground.
Each step sits inside the one before: domain › kingdom › phylum › class › order › family › genus › species. Fungi and plants are separate kingdoms; neither sits under the other.
Non-living nature
From small to large: elements combine into ordered crystals to make minerals, and minerals come together to make rocks. Tap the branches to open each stone’s path.
Minerals199
Naturally 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.
Sulfides and sulfosalts21
Compounds of metals with sulfur; the main ores of many metals.
Halides5
Minerals built with chlorine, fluorine and similar elements: rock salt, fluorite.
Oxides and hydroxides36
Compounds of metals with oxygen: corundum, hematite, quartz (in Nickel-Strunz).
Carbonates and nitrates14
Calcite, dolomite, malachite… Many fizz in dilute acid.
Borates6
Boron minerals. The world’s largest boron deposits are in Türkiye.
Sulfates16
Gypsum, baryte, celestine…
Silicates81
Built from silicon–oxygen tetrahedra, the largest class, making up most of Earth’s crust.
Nesosilicates19
Isolated tetrahedra: olivine, garnet, zircon, topaz.
Sorosilicates5
Paired tetrahedra: epidote, zoisite (tanzanite).
Cyclosilicates12
Rings: beryl (emerald), tourmaline.
Inosilicates15
Chains: pyroxenes, amphiboles, jade.
Phyllosilicates12
Sheets: micas, talc, clay minerals, meerschaum.
Tectosilicates18
Frameworks: feldspars, zeolites.
Rocks64
Natural aggregates of one or more minerals (sometimes glass or organic matter). Rocks are divided into three great groups by how they form.
Igneous rocks25
Formed when molten rock (magma or lava) cools and solidifies.
Intrusive (plutonic)11
Cooled slowly deep underground, coarse-grained: granite, gabbro.
Extrusive (volcanic)13
Cooled quickly at the surface, fine-grained or glassy: basalt, andesite, obsidian.
Sedimentary rocks23
Formed from accumulated and hardened fragments, chemical precipitates or the remains of living things.
Chemical and biochemical10
Precipitated from water or built from shells: limestone, travertine, rock salt.
Metamorphic rocks16
Formed when existing rocks are transformed by heat and pressure without melting.
Foliated7
Minerals aligned in layers: slate, schist, gneiss.
Non-foliated9
Massive, without layering: marble, quartzite.
Mineraloids8
Natural substances that resemble minerals but lack an ordered crystal structure: opal, volcanic glass.
Meteorites and impact stones13
Stones and masses of metal that fell to Earth from space, and the glasses that large impacts created on Earth.
Stony meteorites7
Made mostly of silicate minerals; most meteorites that fall belong here.
Iron meteorites1
Made of iron–nickel alloy; pieces of the cores of shattered planetesimals.
Stony-iron meteorites2
Roughly equal mixtures of metal and silicate; pallasites belong here.
Impact glasses3
Not meteorites: formed from Earth rocks melted and flung out by large impacts (tektites).
Everyday names15
Not scientific species but things we call “stone” in daily life: paving stones, gravel, sand, soil, crushed stone… Each linked to the rocks and minerals it is made of.
- Native metals: Gold, Silver, Copper, Platinum are both metals and minerals.
- Ore minerals: most metals occur in nature not pure but in compounds: Hematite → iron, Chalcopyrite → copper, Galena → lead.
- Ice is a mineral; liquid water is not. Mercury counts as a mineral as an exception, although it is liquid. Coal is a rock.
From living to non-living: what living things leave behind
Substances that living things make or leave behind become part of non-living nature. Some stay buried for millions of years and are transformed by heat and pressure.
Organic gems6
Stones produced by living things or formed from their remains: amber, pearl, coral, jet (Oltu stone).
Common mix-ups
Sources
- Woese, Kandler & Wheelis (1990): three-domain system
- IMA–CNMNC List of Minerals (September 2026)
- TDK Güncel Türkçe Sözlük: “taş”, “kayaç”
- Wikipedia: Classical element
- Wikipedia: Chemical element
- Wikipedia: Fire
- Wikipedia: Atmosphere of Earth
- Wikipedia: Composition of the human body
- Wikipedia: Mineral
- Wikipedia: Native metal
- Wikipedia: Fungus
- Wikipedia: Lichen
- Wikipedia: Virus
- Wikipedia: Human (taxonomy)
- Wikipedia: Coal
- Wikipedia: Petroleum
- Wikipedia: Natural gas
- Wikipedia: Soil
- Wikipedia: Cork (material)