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Forbidden Archeology_ The Full Unabridged Edition - Michael A. Cremo [123]

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“workmanship” on the flakes pictured in these drawings (Figures 3.20, 3.21) hardly approaches that of even the crudest of eoliths.

The quotation from Sollas (1911) about Breuil’s pseudoeoliths continued: “They display just the same forms as other Tertiary ‘eoliths,’ ranging from the obviously purposeless to those which simulate design and bear bulbs of percussion and marginal retouches. Among the most artificial looking are a few which present an astonishing degree of resemblance to special forms of genuine implements; attention may be directed to two in particular, which are compared by the Abbé Breuil, the one to Azilio-Tardenoisian flakes, and the other to the small burins of Les Eyzies; in their resemblance to artificial forms these simulacra far transcend any ‘eoliths’ which have been found on other horizons of the Tertiary series” (Wright 1912, p. 341). Sollas implied that Breuil found at Clermont examples such as these last two, with flakes in place. There is, however, a little dishonesty in this presentation. Sollas should have mentioned that although some pieces of flint were found with flakes lying nearby, these were, although displaying, in some cases, bulbs of percussion and secondary chipping, decidedly nonimplemental in character. Of course, most of the blame lies with Breuil, who wrote the original report.

Sollas concluded: “On the important question of man’s first arrival on this planet we may for the present possess our minds in peace, not a trace of unquestionable evidence of his existence having been found in strata admittedly older than the Pleistocene” (Wright 1912, pp. 341–342). This view is still prominent today, although there are hundreds of discoveries, a good many of which are discussed in this book, that invalidate it.

The case of Wright and Sollas shows how researchers who share a certain bias (in this case a prejudice against evidence for Tertiary humans) cooperate by citing a poorly constructed “definitive debunking report” (in this case by Breuil) as absolute truth in the pages of authoritative books and articles in scientific journals. It is a very effective propaganda technique. After all, how many people will bother to dig up Breuil’s original article, in French, and, applying critical intelligence, see for themselves if what he had to say really made sense?

3.4.7 Breuil Supports Moir

It is interesting to note that Breuil’s “definitive” 1910 report came before most of J. Reid Moir’s discoveries in East Anglia. Eventually, when Moir’s finds began to attract considerable attention, Breuil, and other scientists, went to England to conduct firsthand evaluations. Surprisingly enough, Breuil backed Moir.

M. C. Burkitt (1956, p. 107) wrote: “Messrs Breuil and Boule, who came over to see the finds, still maintained their skeptical attitude. Mr. Moir, however, was undaunted and continued his researches at new sites until finally at Foxhall, a few miles from Ipswich, he collected a series of specimens of such a nature that an examination of them by M. Breuil caused him to change his ideas completely and to join the ever-growing company of those prehistorians who believed in the existence of man as early as late tertiary times.”

It is noteworthy that such a conservative and cautious researcher as Breuil should have come out in favor of Moir. During his visit to England, Breuil had specifically searched Moir’s sites for any evidence of soil movement and pressure. But he found none. George Grant MacCurdy, director of the American School of Prehistoric Research in Europe, wrote in Natural History: “Breuil is authority for the statement that conditions favoring the play of natural forces do not exist in certain . . . deposits of East Anglia, where J. Reid Moir has found worked flints” (MacCurdy 1924b, p. 658).

Some of these deposits are found in the middle of the Red Crag at Foxhall. About Foxhall, Breuil (1922, p. 228) stated: “There is a twin layer in the superior part of the Red Crag, representing without doubt land surfaces that temporarily emerged shortly before the final retreat of the sea

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