In 1996 work began on the systematic
open-area excavation of the whole site. This is a substantial undertaking,
by the far the largest piece of archaeological excavation ever carried
out on the Island. It is also one made more difficult by the fact that
glacial till is amongst the most intractiable type of subsoil to work on
in terms of the legibility of archaeological features.
Having
extensively sampled the topsoil during the field evaluation, the excavation
trenches were mechanically stripped of cultivated soil. Below this level all
excavation is undertaken by hand. As is usual on prehistoric sites, the relationships
between features depends heavily on horizontal stratigraphy, although at Billown
there is considerable intercutting of features and in a few places vertical
stratigraphy still survives. At this stage in the Project, post-fieldwork
analysis is still rudimentary and aimed at constantly refocusing data-collection
for the next season's work rather than general synthesis. This particularly
applies to the environmental sampling of carbonized plant remains and buried
soils. However, it is clear that there was activity on the site, although
not necessarily continuously, from about 5000 Cal BC through to about Cal
AD 600. The evidence for this is briefly summarized in the following subsections
according to conventional cultural-historical periodization.