Coal
Coal consists mostly of carbon but also contains smaller trace amounts of hydrogen, sulfur, oxygen and nitrogen. As a sedimentary rock, coal was initially formed millions of years ago and began as plant matter. Over time, the plant matter decayed into peat, where layers of sediment built up over time, creating an increase in pressure and temperature. This build up causes the peat to undergo chemical and physical changes, stripping it of moisture and stabilizing it – this is known as the coalification process. The importance of coal comes from its versatile nature, being used for many applications such as power generation, industrial fuel, as well as by-products such as tar and ammonia.






































