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Coal Characterization, Its Mining Impacts, Types and its Distribution
Coal is a combustible black or brownish-black sedimentary rock usually occurring in rock strata in layers or veins called coal beds or coal seams. The harder forms, such as anthracite coal, can be regarded as metamorphic rock because of later exposure to elevated temperature and pressure. Coal is composed primarily of carbon, along with variable quantities of other elements, chiefly hydrogen, sulfur, oxygen, and nitrogen.[1] A fossil fuel, coal forms when dead plant matter is converted into peat, which in turn is converted into lignite, then sub-bituminous coal, after that bituminous coal, and lastly anthracite. This involves biological and geological processes that take place over time.
Coal is one of the world’s major sources of energy. Coal is used to produce nearly half of all the electrical energy that is generated and used in the United States. Coal is a very complex and diverse energy resource that can vary greatly, even within the same deposit. In general, there are four basic varieties of coal, which are the result of geologic forces having altered plant material in different ways.
- ACAA (American Coal Ash Association), 2005. 2005 Coal Combustion Product (CCP) Production and Use Survey
- AGI (American Geological Institute), 1997. Dictionary of Mining, Mineral and Related Terms, 2nd ed. Alexandria, Va.: American Geological Institute.
- Averitt, P., 1975. Coal Resources of the United States, January 1, 1974. U.S. Geological Survey, Bulletin 1412; Washington D.C.: U.S. Department of Interior; 131 pp.
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