Abstract
There were two main sources of supply of flint available to early man,–superficial deposits whether in the form of river gravels, sea or lake beaches, or nodules incorporated in surface soils, and deposits beneath the surface of the ground for which it was necessary to mine or quarry. While it is generally true to say that mined flint was of superior quality and more easily worked than the superficial variety it must not be forgotten that the magnificent honey-coloured flint of Grand Pressigny, which in the dawn of the first age of metal was traded to Switzerland, North France, Brittany, Belgium and even Wessex, occurs naturally in the form of surface nodules. In passing it may be observed that the so-called livres de beurre, the most typical product of these Chalcolithic workshops, are technically no more nor less than elongated tortoise-cores from which were struck long flakes with faceted butts. In view of the play that has been made with the presence of ‘Mousterian’ technique in our British mines this is not without its significance.
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