An important step in our knowledge of the British Lower Palaeolithic has been the finding that its two recognized components, ‘Clactonian’ and ‘Acheulean’, are not ranged into a simple sequence; the exact relationship between the two is the subject of much debate. What does this do to interpretations of Swanscombe, classic site of the Lower Thames Valley, which has been studied in terms of stratigraphic succession?
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