Swanscombe: A Standard Stone-Age Sequence for Britain?

In the early twentieth century, Palaeolithic research seemed to be flourishing on the Continent. Commont was carrying out groundbreaking work in the Somme, and rich hauls were being recovered from the reindeer-caves of France and Spain. France could also boast a research centre: the Institute of Human Palaeontology, where Boule, Breuil, and Obermaier held posts. Britain, though, was weighed down by nostalgia: unfavourable contrasts were being drawn between current research and the glorious decades of the past when Evans and Prestwich had brought such renown to British investigations. This apparent loss of impetus was noted abroad. Boule considered the British to have sunk into insularity after 1875, never to regain their early brilliance; in 1912, Breuil remarked at a luncheon party in Cambridge that no one in England knew anything about prehistory. The British Museum’s Guide to the Antiquities of the Stone Age, published in 1911 at the height of Commont’s work, declared: ‘the French system has now been revised in the light of recent discoveries, and is the basis of all Continental classifications’. It was regretted that the English river drifts had still not received any systematic excavations, and that the implements in these sediments still lay in confusion. This Guide was produced by Reginald Smith of the British Museum under the direction of Charles Hercules Read (1857–1929). In 1912, the same year that Breuil made his disparaging comment, Read arranged for Smith to excavate in one of the most productive Palaeolithic localities of the Thames Valley: Swanscombe village. Smith was assisted by Henry Dewey (1876–1965) of the Geological Survey, but the negotiations that gained Dewey’s help would also reveal differences of opinion between their two respective institutions about the value of Palaeolithic research. The connections drawn by Smith to the Continental sequence after working at Swanscombe would lift the gloom about British backwardness. These connections would also help draw the Palaeolithic and geological sequences closer together.