This volume is an integrated overview and synthesis of available data relating to the Quaternary evolution of the River Trent. It provides detailed descriptions of the Pleistocene sedimentary records from the Trent, its tributaries and related drainage systems - a sedimentary record that spans a period of approximately half a million years - and the biostratigraphical and archaeological material preserved therein. Significant new data are presented from recently discovered sites of geological and archaeological importance, including previously unrecognised fluvial deposits, as well as novel analyses, such as mathematical modelling of fluvial incision as recorded by the river terrace deposits. In combination with a thorough review of the literature on the Trent, these new data have contributed to revised chronostratigraphical and palaeogeographical frameworks for central England and revealed the complexity of the Pleistocene fluvial and glacial records in this region. The fragmentary Trent terrace sequence is an important element of wider reconstructions of Pleistocene palaeodrainage in Britain, providing a link between the records preserved in the English Midlands and those in East Anglia.

This edited book presents a novel collection of field-based empirical studies on the Quaternary geomorphology of the Lower Ganga Basin. The book covers a wide range of topics discussing various geomorphological facets of the Lower Ganga and its subsidiary rivers focussing on laterites, palaeoenvironment and palaeogeomorphology, palaeo-coastal landforms, neo-tectonism, tidal-fluvial dynamics, extra-channel geomorphology and channel-pattern adjustment among others. Various methodologies were applied ranging from historical records and religious texts to state-of-the-art remote sensing and GIS techniques. The book appeals to all scientists and post-graduate students of geomorphology and related areas who want to acquire detailed knowledge of the geology and geomorphology of the Lower Ganga Basin or are in search of new methodologies for studying the feedback mechanisms between forms and processes.

The Engineering Group of the Geological Society Working Party brought together experts in glacial and periglacial geomorphology, Quaternary history, engineering geology and geotechnical engineering to establish best practice when working in former glaciated and periglaciated environments. The Working Party addressed outdated terminology and reviewed the latest academic research to provide an up-to-date understanding of glaciated and periglaciated terrains. This transformative, state-of-the-art volume is the outcome of five years of deliberation and synthesis by the Working Party. This is an essential reference text for practitioners, students and academics working in these challenging ground conditions. The narrative style, and a comprehensive glossary and photo-catalogue of active and relict sediments, structures and landforms make this material relevant and accessible to a wide readership.

Associating ice masses with the transport and deposition ofsediments has long formed a central theme in glaciology and glacialgeomorphology. The reason for this focus is clear, in that icemasses are responsible for much of the physical landscape whichcharacterizes the Earth's glaciated regions. This association alsoholds at a variety of scales, for example, from the grain-sizecharacteristics of small-scale moraines to the structuralarchitecture of large-scale, glacigenic sedimentary sequences inboth surface and subaqueous environments. This volume brings numerous state-of-the-art research contributionstogether, each relating to a different physical setting, spatialscale, process or investigative technique. The result is a diverseand interesting collection of papers by glaciologists, numericalmodellers and glacial geologists, which are all linked by the themeof investigating the relationships between the behaviour of icemasses and their resulting sedimentary sequences.

The papers in this volume came out of a symposium focusing on mining and its wider impact, at the 66th Annual Meeting of the Society for American Archaeology. A number of fundamental questions were posed to the presenters, including: did the raw mined material have a symbolic value?, were the mines considered special places? were the miners craft specialists? did they have a particular social niche? In the wider landscape perspective, it was hoped that the case studies would also throw some light upon the choices of site locations: were mines and quarries simply positioned at the most convenient source of raw material, or were other considerations such as quality, rarity or colouration involved? Arguably the special nature of certain mining locations was linked to the local communities worldview, they must have been associated with traditional stories and oral histories. The presence of graffiti or rock art can often betray a 'special' location. Similarly, assemblages of carefully placed artefacts or pottery can also reveal specialised deposition, even amongst relatively mundane 'functional' tool types. Finally, the rare occurrence of burials in some mines and quarries offers further perspectives on how these sites may have been perceived by contemporary communities. The archaeological record does suggest a multiplicity of activities were focussed upon some mining sites, which do not easily fit with interpretations of extraction strategies. Although it could never be effectively argued that all mining had ritualised or ceremonial undertones, in some cases there was a definite and demonstrable special nature to the mining activity: this book presents some of those case studies.(Oxbow Books 2004)

A detailed account of the geology shown on the complementary 1: 50 000 (or earlier 1: 63 360) geological map(s)

In describing the geomorphological heritage of Scotland, this volume offers a remarkable account of how the natural environment responded in terms of landforms, processes and plant communities, to severe climatic change as the Quaternary era progressed over the last two million years. This legacy, as preserved in the 138 nationally important GCR sites described, documents a remarkable diversity of landforms in a relatively small area. The rugged highland contrast with the rolling hills and flat plains found further south, while the western and northern islands, together with the highly-indented coastline add further to the scenic diversity. How this variety of landscapes came into being, the forces which shaped it , and the climatic extremes which drove it, are the themes explored in this volume.

Edited by Pierre Allard, Françoise Bostyn, François Giligny and Jacek Lech This book includes papers from the Flint Mining in Prehistoric Europe session held at European Association of Archaeologists 12th Annual Meeting Cracow, Poland, 19th-24th September 2006.