Abstract
The crust of the earth is about 30–70-km-thick form of the outer layer of the planet in which all rocks and minerals are found. Beneath the crystal layer is the zone known as the Mohorovičić discontinuity , which is followed by heavy rocks of a thickness of 3000 km. This is followed by a 1800-km-thick outer core of iron and nickel in a hot semi-plastic condition, which in turn is followed down to the centre by an inner core of 1000 km thickness.
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Roonwal, G.S. (2018). Composition of the Earth and Mineral Resources. In: Mineral Exploration: Practical Application. Springer Geology. Springer, Singapore. https://doi.org/10.1007/978-981-10-5604-8_2
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DOI: https://doi.org/10.1007/978-981-10-5604-8_2
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