The earlier work made it essential that something be done about the site when the threat of gravel-digging arose in the late 1950s. Today a threat of this sort to an archaeological site would lead to a dig which would be funded by the company that owned the gravel quarry – which is fair, as it is they who stand to profit from the site’s destruction. But in those days there was less justice, and the local archaeologists had to find the money, which they managed to do, from the local museums, the Prehistoric Society and Cambridge University. The Prehistoric Society, incidentally, is the national society for the study of all pre-Roman archaeology. Its Proceedings is an academic journal of record, and is pretty technical. But it also organises tours of prehistoric landscapes in Britain and Europe, and has regular meetings, a wide non-professional membership, and a lively newsletter, Past.18 The Society helped to excavate Thatcham – and dozens of other sites in Britain.
As a first stage, John Wymer decided to cut a quick reconnaissance or trial trench in December 1957. This produced quantities of flint and scraps of bone which lay beneath nine inches (twenty-three centimetres) of peat and eighteen inches (forty-six centimetres) of peaty topsoil. This depth of material was hugely important, because it meant that the site beneath was sealed intact. It could never have been damaged by ploughing, and the presence of the in situ peat bed clearly demonstrated that it hadn’t. John immediately realised that he had an extraordinarily important site on his hands.
As work progressed in the seasons that followed that winter exploratory trench, it became evident that Thatcham was not just one site. It was clearly a place where people settled repeatedly, as there were distinct concentrations of flint and other debris on the gravel terrace that ran along the river. Although many flint implements were made there, Thatcham doesn’t seem to have been a place where specialised tasks were carried out, like the antler-working at Star Carr. And there was a huge variety of things found: antler and bone, as at Star Carr, hammerstones for flint-working, flint axes or adzes and vast numbers (16,029) of waste flakes, blades (1,207), cores (283) and those tiny, geometrically-shaped microliths (285) that were used to make composite spears and arrowheads. At Thatcham waste flakes formed 96.5 per cent of the entire flint assemblage, even higher than at Star Carr (92.8 per cent).
John’s style of excavation was rather like that of Stephen Aldhouse-Green, somewhat more recently. Both are neat and extremely meticulous, and both make a point of recording everything they find three-dimensionally. This takes time and effort; it also only happens if the crew actually doing the work are happy and highly motivated – and that’s the real skill of a successful dig director: somehow he must keep people informed and enthusiastic, otherwise they won’t willingly do what he asks them.
The most important concentration of occupation debris at Thatcham was unearthed in an area known as Site III, where John had not expected to find much. Like the other settlement sites it was located on the edge of a slope which dipped down to reed beds along an edge of the river floodplain. In Mesolithic times it would have been on the edge of a large lake. The area in question was actually a shallow dip when seen from the surface, and John had quite reasonably expected to find better evidence for settlement on the drier humps than in the damper hollows. But in this case his guess was wrong, which, paradoxically, is why he is such a good field archaeologist. A lesser man would only have put trenches where he expected to make discoveries. A good archaeologist, however, is always aware that he must break the mould, destroy the predictable chains of reasoning.
Like other sites at Thatcham, Site III was dug by yard (metre) squares, and flints were recorded to the appropriate square. As the crew worked they were amazed by the density of flints they found: sometimes as many as two to three hundred per square, and in one extraordinary instance a massive 764. In amongst the flints were numerous burnt pebbles, burnt and unburnt bones, burnt hazelnuts and spreads of charcoal, clear evidence for hearths or fires – and indeed for food, both meat and nuts. This was clearly a domestic site, and clearly too it had been occupied more than once, because some of the flints showed signs of having been worked twice. The sheer quantity of material also indicated repeated use of the place.
There were also some areas of Site III where there were low densities of flints. If we plot the densities at Site III, we notice that there’s an area near the centre of the site which is relatively free from flints and surrounded also by hearths. If one assumes that flint-working was an activity best carried out in the open (as we saw, for example, at Boxgrove), this could well have been a place where light structures were erected when people returned to the site. It measures about 6.5 by 5.5 metres, and has a floor area of some thirty-five square metres – large enough for a single family. In northern Europe there is evidence that early postglacial people made houses by bending birch saplings and covering them with hides. These are about the same size as the possible house-sized space at Thatcham.
It seems probable that more than one family occupied the ridge at Thatcham, and that, like other communities of the time, they were mobile. Their home-base was probably occupied in the summer months, and analysis of pollen shows it to have been positioned within birch woodland, on the edge of the lake.19 They hunted a variety of animals, including both native species of deer, and wild pig (a term I prefer to ‘wild boar’, which implies that all the animals are male) was particularly important.
Once in a while it happens that an archaeologist excavates a site and publishes a report in which he speculates about its date and function, then someone else comes along ten years later, with the improved techniques of the time, and proves him right or wrong. It happened to me a few years ago, and I was proved wrong – but in the nicest possible way.20 It happened to John Wymer too – and of course he was proved right. Another spread of flint on the same ridge, but about two hundred metres to the north-west, was excavated in 1989.21 This revealed a pattern of sharp rises and falls in the density of flints found on the ancient surfaces, just as John had done, but the excavators now had available the newer technique of microwear, or use-wear, analysis. Essentially this is a way of examining microscopic damage to the scraping and cutting edges of flint tools, but it requires flints from sealed contexts, such as Thatcham (where the occupation levels were covered by a layer of peat), otherwise it’s hard to discount the ‘noise’ caused by more recent, post-depositional effects, such as plough damage.
The technique relies on the controlled experimental ‘use’ of flints, which are then examined, and the results compared with the ancient material. The microscopic edge-damage found at kill or butchery sites is very characteristic and includes, as one might expect, evidence for percussion and harsh damage, when joints are severed and bones are broken. There will also be arrowheads and projectile points at such sites. A domestic site – a home-base, in other words – produces a far more diverse pattern of edge-wear. The heavy-duty percussive damage tends to be lacking, as are quantities of arrowheads, and there are more signs of scraping hides and sinews, and of cutting soft materials, such as vegetable matter. The range of flint implements found at Thatcham, and the edge-wear revealed in the microwear analyses, showed that it had indeed been a domestic site. John had been right: it was a true home-base.
It cannot have escaped attention that up till now I have been writing about Britain alone – as if Ireland was floating out over the horizon, miles away in the Atlantic. Of course it wasn’t, but neither was it inhabited by human beings in the Ice Age, with the possible exception of the odd visitor or two at the close of the Lower Palaeolithic.22