This two volume monograph about the region of Thy in the early Bronze Age provides a high resolution archaeological and ecological model of the organisation of landscape, settlements and households during the period 1500-1100 BC. Bordering the North Sea to the west, and the calmer waters of the Limfjord to the east, the region of Thy in Denmark experienced four centuries of intense economic and demographic expansion. By combining results from environmental and economic research (pollen and palaeo-botanical analyses) with intensive field surveys and excavations of farmsteads with exceptional preservation, it has been possible to open a window to the changes that transformed Bronze Age society and its environment during a few centuries of exceptional expansion and wealth consumption. The results from this interdisciplinary venture made it possible to link together the histories of local farmsteads with the wider regional and global history of the Bronze Age in North-western Europe during this period. Here is much to feed on for students and researchers of the Bronze Age alike.

First Published in 2004. This book is both a survey of Danish prehistory and a detailed presentation of the problems, themes and literature of modern Danish archaeology. It was written to present a general survey of the prehistory of Denmark as it has emerged after the past decade of research. The book is composed of four sections: The hunters and gatherers, the first farmers, towards a new era and the chiefdom of the Iron Age. Each section includes chapters dealing with the environment, demography, subsistence patterns and social patterns. Each section is followed by a survey of the archaeological record for the period and a discussion of the relevant literature. The book concludes with a bibliography of approximately 700 titles covering most of the major Danish archaeological studies since about 1950.

Accompanying CD-ROM contains fold. col. map, entitled, in both formats, "Caledonian orogen : East Greenland 70°N-82°N : Geological map 1:1 000 000.

Glacially triggered faulting describes movement of pre-existing faults caused by a combination of tectonic and glacially induced isostatic stresses. The most impressive fault-scarps are found in northern Europe, assumed to be reactivated at the end of the deglaciation. This view has been challenged as new faults have been discovered globally with advanced techniques such as LiDAR, and fault activity dating has shown several phases of reactivation thousands of years after deglaciation ended. This book summarizes the current state-of-the-art research in glacially triggered faulting, discussing the theoretical aspects that explain the presence of glacially induced structures and reviews the geological, geophysical, geodetic and geomorphological investigation methods. Written by a team of international experts, it provides the first global overview of confirmed and proposed glacially induced faults, and provides an outline for modelling these stresses and features. It is a go-to reference for geoscientists and engineers interested in ice sheet-solid Earth interaction.