When plants and trees died their remains sunk to the bottom of the swamps and as layers built up they formed a dense, soggy material called peat. After millions of year’s layers of sediment became compacted, much of the water removed and coal was formed. This is the reason coal is so flammable because of there are lots of trees compressed into one small piece of coal. This means that the coal is high in carbon; it is the carbon that is burnt therefore, producing large quantities of heat. There are four different types, which are peat, lignite, black coal and anthracite. Peat is used as a domestic fuel in rural parts of Scotland and Ireland. It contains roots of plants and shows very little alteration. Lignite is very young coal (upwards of around 40,000 years). It is brown and can be soft and fibrous containing plant material. It has a lot of moisture and low energy content. As lignite develops from peat it loses its fibrous character and darkens in colour. Black coal was formed around cretaceous age (65 to 105 million years ago) to mid Permian age (up to 260 million years ago). It is black and very sooty but still very high in moisture. Anthracite is very hard, black and shiny. It contains virtually now moisture and very low volatile