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Coal is a carbon-rich sedimentary rock formed over millions of years, and the coal industry has played a significant part in global energy, industrial development, and environmental policy.

Coal is a combustible black or brownish-black sedimentary rock composed largely of carbon and hydrocarbons, formed from ancient plant material buried under layers of sediment. Over millions of years, heat and pressure transformed this organic matter into coal, a process known as coalification.

Coal is considered nonrenewable because its formation spans geological timescales. The energy stored in coal originates from plants that lived in prehistoric swamp forests, whose remains were compacted and chemically altered into progressively higher-rank coals.

Coal has been used since antiquity. Archaeological evidence shows coal burned in Bronze Age Wales, and classical authors such as Aristotle and Theophrastus described its use. The Romans in Britain used coal for heating, and by the Middle Ages, coal was mined in northern England. In North America, the Hopi people mined and used coal as early as the 12th century. Coal's global significance surged during the Industrial Revolution, when it became the primary fuel for steam engines, metallurgy, and early electricity generation. Although petroleum and natural gas overtook coal in the mid-20th century, coal remained a major global energy source.

Coal is classified into four ranks, based on carbon content and heating value. Anthracite coal(86-97% carbon) has the highest energy content and is used mainly in the metals industry. Bituminous coal (45-86% carbon) is the most abundant in the United States, and is used for electricity generation and as coking coal in steelmaking. Subbituminous coal (35-45% carbon) has a lower heating value and is widely used for electric power generation. Lignite coal (25-35% carbon) is the lowest rank and has a high moisture content; it is used in mine-mouth power plants. These ranks reflect increasing heat and pressure during coalification, with higher-rank coals producing more energy per unit mass.

Coal remains abundant, with major reserves in the United States concentrated in Wyoming, Montana, West Virginia, Pennsylvania, and Illinois. U.S. coal production peaked in 2008, and consumption in 2007, followed by a long decline driven by competition from natural gas and renewables, as well as plant retirements. Employment in the coal sector has fallen 92% over the past century, even as mining efficiency increased.

Coal is mined through surface and underground methods, both now highly mechanized. Surface mining dominates in the western United States, while underground mining remains common in Appalachia.

Coal's environmental impacts are significant. Coal consumption is a major source of CO2, contributing to climate change. Burning coal releases sulfur dioxide, nitrogen oxides, particulates, and mercury, affecting air quality and public health. Surface mining alters landscapes, while underground mining can cause subsidence and water contamination. Coal ash contains heavy metals requiring disposal. These concerns have accelerated the shift toward cleaner energy sources and stricter environmental regulations.

Topics relating to coal, the coal industry, and its use as a source of energy and utilities are the focus of this category.

 

 

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