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  2. Coal - Wikipedia

    en.wikipedia.org/wiki/Coal

    Subbituminous coal can form at temperatures as low as 35 to 80 °C (95 to 176 °F) while anthracite requires a temperature of at least 180 to 245 °C (356 to 473 °F). [24] Although coal is known from most geologic periods, 90% of all coal beds were deposited in the Carboniferous and Permian periods. [25]

  3. Carboniferous - Wikipedia

    en.wikipedia.org/wiki/Carboniferous

    Coal forms when organic matter builds up in waterlogged, anoxic swamps, known as peat mires, and is then buried, compressing the peat into coal. The majority of Earth's coal deposits were formed during the late Carboniferous and early Permian. The plants from which they formed contributed to changes in the Carboniferous Earth's atmosphere. [25]

  4. Fossil fuel - Wikipedia

    en.wikipedia.org/wiki/Fossil_fuel

    In 2000, about 12,000 tonnes of thorium and 5,000 tonnes of uranium were released worldwide from burning coal. [47] It is estimated that during 1982, US coal burning released 155 times as much radioactivity into the atmosphere as the Three Mile Island accident. [48] Burning coal also generates large amounts of bottom ash and fly ash.

  5. Geology of the Peak District National Park - Wikipedia

    en.wikipedia.org/wiki/Geology_of_the_Peak...

    The geology of the Peak District National Park in England is dominated by a thick succession of faulted and folded sedimentary rocks of Carboniferous age. The Peak District is often divided into a southerly White Peak where Carboniferous Limestone outcrops and a northerly Dark Peak where the overlying succession of sandstones and mudstones dominate the landscape.

  6. Permineralization - Wikipedia

    en.wikipedia.org/wiki/Permineralization

    A coal ball. Carbonate mineralization involves the formation of coal balls. Coal balls are the fossilizations of many different plants and their tissues. They often occur in the presence of seawater or acidic peat. Coal balls are calcareous permineralizations of peat by calcium and magnesium carbonates. Often spherical in shape and ranging from ...

  7. Seatearth - Wikipedia

    en.wikipedia.org/wiki/Seatearth

    Seatearth is a British coal mining term that is used in the geological literature. As noted by Jackson, [ 1 ] a seatearth is the layer of sedimentary rock underlying a coal seam. Seatearths have also been called seat earth , "seat rock", or "seat stone" in the geologic literature.

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  9. Coke (fuel) - Wikipedia

    en.wikipedia.org/wiki/Coke_(fuel)

    Raw coke. Coke is a grey, hard, and porous coal-based fuel with a high carbon content. It is made by heating coal or petroleum in the absence of air. Coke is an important industrial product, used mainly in iron ore smelting, but also as a fuel in stoves and forges.

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