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In the beginning

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Abstract

The Earth is old, and in its fabric is written a subtle and complex history. The oldest material ever discovered on Earth consists of a few crystals of a mineral called zircon. These crystals, found in Western Australia, are about 4.3 billion years old. Many of the elements that make up the Earth are roughly 4.6 billion years old, and the planet probably formed soon after that, although much of thç hydrogen in our water may be as old as the universe. For the first 300 million years that Earth existed there is no history recorded in our terrestrial rocks, although the Moon, meteorites and comets preserve earlier material. Some meteorites even preserve traces of events that took place before the formation of the Solar System.

A zircon crystal from Western Australia, 4.15 billion years old. This crystal, and others like it that range up to nearly 4.3 billion years old, formed a few million years after the accretion of the Earth. Scale bar is 100 microns long (courtesy of W. Compston).

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Further Reading

  • Broecker, W. 1985. How to build a habitable planet. New York: Lamont Doherty Geological Observatory of Columbia University, Eldigio Press.

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  • Brown, G.C. & A.E. Mussett 1981. The inaccessible Earth. London: Allen & Unwin.

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  • Cloud, P. 1978. Cosmos, Earth and man. New Haven: Yale University Press.

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  • Fowler, C.M.R. 1990. The solid Earth. New York: Cambridge University Press.

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© 1991 Springer Netherlands

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Nisbet, E.G. (1991). In the beginning. In: Living Earth. Springer, Dordrecht. https://doi.org/10.1007/978-94-011-3056-1_1

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  • DOI: https://doi.org/10.1007/978-94-011-3056-1_1

  • Publisher Name: Springer, Dordrecht

  • Print ISBN: 978-0-04-445855-5

  • Online ISBN: 978-94-011-3056-1

  • eBook Packages: Springer Book Archive

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