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How does coal form?
Quick answer
Coal forms from ancient swamp plants. When they die, peat accumulates underwater, where low oxygen slows decay. Burial under sediment compresses the peat and raises its temperature. Over millions of years, heat and pressure expel water and gases, leaving a carbon-rich rock that progresses from lignite to bituminous coal to anthracite.
Coal forms when dead plant material accumulates in swamps, is buried under sediment, and is slowly transformed by heat and pressure over millions of years. This process, called coalification, concentrates carbon and drives off water and gases, turning peat into lignite, then bituminous coal, and finally anthracite.
Step by step
- Plants die and fall into waterlogged swamps, where low oxygen prevents full decay and peat accumulates.
- Sediment like mud and sand washes over the peat, burying it deeper and deeper over time.
- Increasing burial depth raises temperature and pressure, squeezing water and volatile gases out of the peat.
- The remaining material becomes progressively richer in carbon, transforming from peat to lignite to bituminous coal.
- With deeper burial and higher temperatures, bituminous coal turns into hard, shiny anthracite, the highest rank of coal.
Key things to understand
- Coal begins as peat, a soggy layer of partly decayed plants that builds up in waterlogged swamps where oxygen is scarce.
- When mud and sand bury the peat, rising temperature and pressure start driving off water, methane, and carbon dioxide.
- Over millions of years, the buried peat compacts and loses volatiles, gradually increasing its carbon concentration.
- The rank of coal rises through lignite, sub-bituminous, bituminous, and anthracite as burial depth and heat increase.
- Most of the world's coal formed during the Carboniferous Period, roughly 300 to 360 million years ago, when vast swamp forests covered continents.
Labelled diagram
- Peat
Partially decayed plant matter accumulates in waterlogged, low-oxygen swamps.
- Burial
Sediment deposits cover the peat, burying it deeper over thousands of years.
- Compaction
Pressure squeezes out water, and temperature rises with depth, driving off gases.
- Lignite
Soft brown coal forms as carbon content increases and moisture decreases.
- Bituminous
Further heat and pressure create denser black coal with higher carbon content.
- Anthracite
Extreme burial metamorphoses coal into hard, shiny, almost pure carbon.
Real-world examples
- The Appalachian coal fields in the eastern United States were formed from swamp forests during the Carboniferous Period and contain large deposits of bituminous coal.
- The Ruhr region in Germany has deep coal seams that formed during the Carboniferous and supported heavy industry for centuries.
- The Powder River Basin in Wyoming and Montana holds thick seams of sub-bituminous coal that formed from peat swamps about 60 million years ago.
- The Jharia coalfield in India contains bituminous coal that formed during the Permian Period, around 250 to 300 million years ago.
Common mistake
✗ Myth: Coal is made from dead dinosaurs.
✓ Fact: Coal actually forms from ancient plants, mainly ferns, trees, and mosses that lived in swamp forests. While dinosaurs lived during the Mesozoic Era, most coal deposits formed earlier, during the Carboniferous Period, from plant material that accumulated before dinosaurs existed.
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Part of the guide: Nature & Earth: Living Things and Rocks →

