This article results from a series of visits by the authors to the 44 hillforts of south-east England. Our aim was to re-contextualize these hillforts in their landscapes. Analysis of the pottery assemblages and radiometric dates allows a three-phase chronological division of these hillforts. Assessment of the topographic positions and excavated evidence indicates that the enclosures may have functioned in distinctly different ways in each of the three phases. The data for south-east England offer a counter-analysis to the extant ‘Wessex-centric’ view of southern British hillforts.

We present data on the chemical and lead isotope composition of copper and bronze objects from Nuragic Sardinia. The sample suite comprises, inter alia, objects from the hoard finds at Arzachena (21 objects), Bonnanaro (10), Ittireddu (34), and Pattada (20), all in northern Sardinia. With one exception, all ingot fragments (49) consist of unalloyed copper; the exception comes from Ittireddu and contains 11 per cent tin. In contradistinction, all implements (21) are made from standard bronze with a mean tin content of 10.8 per cent. A dozen sword fragments from the Arzachena hoard, all of fairly uniform small size, are pieces of a large number of different swords. The low tin content of only about 1 per cent would have made for poor weapons, confirming the archaeological identification of the fragments as pieces of votive swords. Scrap metal from Arzachena is remarkable for its wide range of trace element contents and lead isotope abundance ratios. It is dissimilar to all other metal samples investigated, possibly representing metal from local smelting experiments using a variety of different copper ores. Lead isotope data and trace element patterns, alone or in conjunction, do not allow us to tell oxhide ingots from plano-convex (bun) ingots. Most ingot fragments have a lead isotope signature similar to those of Cypriot copper ores but there are also a number of ingots whose lead isotope fingerprints are fully compatible with them being local products. Of the bronzes, none has lead with an isotopic composition characteristic of copper ingots from Cyprus. All contain local lead, suggesting the bronze implements were manufactured locally. Isotopically-fitting lead is found in copper and lead ore deposits from the Iglesiente-Sulcis district in south-west Sardinia and from Funtana Raminosa in central Sardinia.

The process of the production of copper and bronze is presented in this paper as a sequential operation. Each stage of this process may influence the final product. The deconstruction of the process is a convenient way of examining each individual stage, using archaeological case studies from different places within the Old World and, where useful, ethnographic studies. The examination will focus on two aspects: innovation and specialization. It seeks to move beyond technological determinism by relating the study of technology to the context of those societies which shaped and practised it and which exercised certain choices in its execution.

The current consensus is outlined about the application of lead isotope analyses to metal provenance studies and to the unravelling of the Mediterranean Bronze Age copper trade, with special reference to copper oxhide ingots. Various misconceptions, especially some of those contained in Knapp (1999, 2000), are corrected. It is shown that there is no need to fall back on hypotheses based upon the Mediterranean-wide mixing/recycling of copper metals to explain the lead isotope characteristics of post-1250 BC copper oxhide ingots, since there is a good isotopic coincidence between these ingots and the Apliki region ore deposits in Cyprus. Weaknesses are exposed in the hypotheses of direct or indirect pooling of Cypriot ores, and of the proposed widespread recycling of metals in a Mediterranean-wide koine, particularly since there is no evidence for a homogeneity of lead isotope composition in artefacts and no tin in the oxhide ingots.