Eolith

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An eolith (from Greek "eos", dawn, and "lithos", stone) is a chipped flint nodule. Eoliths were once thought to have been artefacts, the earliest stone tools, but are now believed to be naturally produced by geological processes such as glaciation.

The first eoliths were collected in Kent by Benjamin Harrison, an amateur naturalist and archaeologist, in 1885 (though the name "eolith" wasn't coined until 1892, by J. Allen Browne). Harrison's discoveries were published by Sir Joseph Prestwich in 1891, and eoliths were generally accepted to have been crudely made tools, dating from the Pliocene. Further discoveries of eoliths in the early 20th century – in East Anglia by J. Reid Moir and in continental Europe by A. Rutot and H. Klaatsch – were taken to be evidence of human habitation of those areas before the oldest known fossils. Indeed, the English finds helped to secure acceptance of the hoax remains of Piltdown man.

Because eoliths were so crude, concern began to be raised that they were indistinguishable from the natural processes or erosion. M. Boule, a French archaeologist, published an argument against the artifactual status of eoliths in 1905 ^[1], and S. Hazzledine Warren provided confirmation of Boule's view after carrying out experiments on flints ^[2].

Although the debate continued for about three decades, more and more evidence was discovered that suggested a purely natural origin for eoliths. This, together with the discovery of genuine late-Pliocene tools in Africa (the Olduwan tools), made support for the artefact theory difficult to sustain.

[edit] References

• Terry Harrison, "Eoliths", in Encyclopedia of Anthropology ed. H. James Birx (2006, SAGE Publications; ISBN 0-7619-3029-9)