Chronologies of the Early Twentieth Century
Dr Allen Sturge spelled out some of the problems facing researchers who worked on the British Palaeolithic in his first Presidential Address to the Prehistoric Society of East Anglia. For the Drift period, the main task was ‘to ascertain the relative ages of the humanly-worked stones, and the number of the periods concerned’.1 In 1908, when Sturge made this suggestion, he was troubled by suspicions that the French divisions—Chellean, Acheulian, and Mousterian—were too broad to encompass the variety of British tools. He called on the younger school of geologists to help solve the dificulty. A few elderly Wgures, familiar from previous chapters, would accompany Sturge’s younger school of geologists as they worked on various sequences that could give a date to the stone tools of Britain. James Geikie published The Antiquity of Man in Europe in 1914, still defending his sequence of interglacials. 2 Harmer was inspired to take up the glacial researches of his old friend Wood as the twentieth century dawned. The refiection left by the Glacial epoch in East Anglia also led the young geologist Percy Boswell (1886–1960) to consider the connections between boulder clays and Palaeolithic industries. Dawkins continued to promote his classification of Quaternary mammals and to attack Geikie’s views, but two newcomers took a different approach to the palaeontological sequence. Martin A. C. Hinton and Alfred Santer Kennard used the bones of smaller mammals and the shells of molluscs to reconstruct the geological history of the Thames Valley. They maintained the traditional antagonism of palaeontologists towards the theories of glacial geologists by suggesting controversial links between the river drifts and the glacial sequence.3 Meanwhile, Warren, the eolith sceptic, developed his own opinions about the British Palaeolithic sequence and its place in geological time as he worked on Palaeolithic sites around Essex. Several different answers to Sturge’s question about the relative ages of stone tools would be extracted with the help of these sequences of glacial deposits, bones and shells, and river sediments.