Coal is a black, hard amorphous form of carbon and the cheapest source of power fuel contributing to almost 40% of the world's electricity production.
The formation of coal goes back to 300 million years ago when the Earth was enveloped with swampy forests.
With the passage of time, the plants, tress, mosses, and ferns died and fell into these swamps resulting in the formation of thick layers of dead vegetation.
After the decomposition of this organic matter under high pressure, high temperature, and absence of air the carbon-rich deposit was formed.
Based on the carbon content present, there are different varieties of coal namely: anthracite, lignite, bituminous, sub-bituminous, and peat.
Among these anthracite bearing the highest rank of coal contains a high concentration of carbon and is hard.
While lignite is the softest and considered as lowest grade coal as it is having low carbon concentration.
Bituminous and sub-bituminous have a moderate level of carbon concentration.