Published online by Cambridge University Press: 21 April 2011
The Lake District mountains have long been known as the source of Neolithic artefacts belonging to petrological group VI. The study of their wider distribution has played a central part in investigations of the ‘axe trade’. Unfortunately, it is not clear that all Group VI axes originated in this area and in any case it is now known that there is no direct relationship between different fall-off patterns and the processes that led to their creation. At the same time, it is not possible to compare work at Neolithic flint mines with current knowledge of how non-flint axes were distributed. Recent fieldwork, in the wake of a survey carried out by the National Trust and the Cumbria and Lancashire Archaeological Unit, has tried to investigate the ways in which stoneworking at Great Langdale was organized and the relationship between methods of exploiting the raw materials on site and changes in the distribution of Cumbrian axes across Britain as a whole. This has involved experimental archaeology, technological analysis, environmental investigations and small-scale excavation. This work has resulted in the recognition of two distinct modes of production. These are discussed in relation to the environmental history of the surrounding region.