



The most abundant pottery fabric, Typical Gabbroic, was made using coarse clay which is mainly found in a 1 km2 area near Zoar. Owing to the unusual geology of the Lizard these groups can be attributed to specific locations. The research uses petrographic and chemical analysis to subdivide the prehistoric pottery into six groups. This analysis of prehistoric pottery and clay samples from Cornwall demonstrates that the clay used to make Cornish gabbroic pottery in prehistory originated around the gabbro rock outcrop in a small area of the Lizard peninsula. Bringing together the Iron Age settlement evidence for the Atlantic regions in one place for the first time, this excellent and original book is certain to establish itself as the definitive study of the Atlantic Iron Age. As a history of these communities unfolds, a general archaeological Atlantic identity breaks down into a range of regional identities which compare interestingly with each other and with traditional models of Celtic identity. A major theme running through the book is the role of the Atlantic seaboard itself and what impact this unique environment had on the ways Atlantic communities perceived themselves and their place in the world. He also pinpoints areas of similarity: the possibility of cultural 'cross-pollination' caused by maritime links and to what extent these contacts influenced and altered the distinctive character of local communities. By examining the evidence for settlement and maritime trade, as well as aspects of the material culture of each area, Henderson identifies distinct Atlantic social identities through time.

Henderson provides an important and much-needed exploration of the archaeology of western areas of Britain, Ireland, France and Spain to consider how far Atlantic Iron Age communities were in contact with each other. This book is the first ever survey of the Atlantic Iron Age: this tradition is cited in archaeology frequently enough to seem firmly established, yet has never been clearly defined.With this book, Jon C.
