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Story: Coal and coal mining

Rank of coal

Rank Moisture
(%)
Volatile matter
(%)
Fixed carbon
(%)
Original depth
of burial (m)
Peat 80 9 5  
Lignite 55 20 17 up to 1,000
Sub-bituminous 20 36 40 up to 2,000
Bituminous 2 36 60 up to 5,000
Semi-anthracite 1 9 87 more than 5,000

The rank of coal is determined by how deeply the original plant matter was buried. Plant material buried close to the surface becomes peat, while plants buried very deeply become semi-anthracite coal. As the depth increases, the proportion of water in the coal decreases and the proportion of carbon increases. These changes also affect the volume of the coal. As it becomes higher in rank, water and gaseous hydrocarbons are driven off, and the coal becomes more compressed.

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Te Ara – The Encyclopedia of New Zealand

Source: GNS Science

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How to cite this page

Alan Sherwood and Jock Phillips, Coal and coal mining – The nature of coal, Te Ara – the Encyclopedia of New Zealand, https://teara.govt.nz/en/table/7408/rank-of-coal (accessed 24 June 2026).

Story by Alan Sherwood and Jock Phillips, published 2 March 2009.