What was happening along the low lying, dry ground alongside the Winterbourne in the Neolithic and Early Bronze Age? And what was happening in the wider landscape at the time Avebury henge was being built over 4,500 years ago?
These questions were in mind when we began excavating the deeply buried prehistoric soils. Excavation was in the chequerboard style (as with Between the Monuments and the Foot of Avebury Down excavations) in order to achieve spatial distribution and density patterns (and, as a bonus, it looks lovely).
©National Trust/Briony Clifton
There was a general, low density scatter of material, and worked flint present in all four trenches.
Much of the flint is from the Early or Later Mesolithic (Early Mesolithic flint is rare for this region). From excavation archives carried out in this area in the 1980s, Mesolithic activity on site was not unexpected; what was unexpected was that the presence of Mesolithic flint work was in all the 2018 trenches.
Among the flint flakes there were a few microliths present, which are characteristic of the Mesolithic period. Microliths are tiny shaped flint flakes which make up composite tools. For the flint fanatics among you it’s possible to recognise the difference between Early Mesolithic microliths and Late Mesolithic ones (four Late Mesolithic ‘rod’ form microliths were uncovered).
Microlith ©Jake Rowland
The discoveries indicate Mesolithic presence in the form of repeated visits and activity, making use of the area by the river that was dry ground. Early and Late Neolithic worked flint was also present on site. It wasn’t as common, but much of it refits and is in situ!
Come back tomorrow to find out about the later archaeology on site…..