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Coal
Coal

Limestone
Limestone



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Formation of Coal and Limestone

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Formation

Formation

Mineral Content

Compound Content

Metamorphism

Types of Metamorphism

Weathering

Types of Weathering

Erosion

Types of Erosion

 
Coal forms from the accumulation of plant debris in a swamp environment which is buried by sediments such as mud or sand and then compacted to form coal.
Analcime, Apatite, Barite, Calcite, Chalcopyrite, Chlorite, Chromite, Clausthalite, Clay Minerals, Crandallite Group, Dolomite, Feldspar, Galena, Gypsum, Marcasite, Muscovite or Illite, Pyrite, Quartz, Siderite, Sphalerite, Zircon
Carbon, Hydrogen, Nitrogen, Oxygen, Sulphur
Burial Metamorphism, Cataclastic Metamorphism, Regional Metamorphism
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Limestone is a sedimentary rock which is mainly made up of calcium carbonate.
Calcite, Chert, Clay, Dolomite, Quartz, Sand, Silt
Aluminium Oxide, NaCl, CaO, Iron(III) Oxide, FeO, MgO
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Biological Weathering, Chemical Weathering, Mechanical Weathering
Chemical Erosion, Coastal Erosion

Coal and Limestone Formation

Formation of rocks is a long process and hence, Coal and Limestone formation sounds very interesting. According to the formation, all rocks are divided into :Igneous Rocks, Sedimentary Rocks and Metamorphic Rocks. Igneous rocks form by crystallization of magma or lava. The magma is made up of various components of pre-existing rocks which have been subjected to melting either at subduction zones or within the Earth's mantle. Igneous rocks are generally seen at mid ocean ridges or in intra-plate hotspots. Sedimentary rocks are formed when sediments accumulate gradually. As the sediments are buried they get compacted as more and more material is deposited on top. Eventually the sediments become so dense that they form a rock. Metamorphic rocks are rocks which once existed as igneous or sedimentary rocks but have been subjected to varying degrees of pressure and heat within the Earth's crust. Get to know all about formation of Coal and Limestone, composition of Coal and Limestone and their transformation.