A memoir describing the sediments and rocks of the coastal region of East Anglia between Lowestoft and Aldeburgh, outlining the history of their formation and discussing their relationship to the present day landscape. The local geology has greatly influenced many aspects of human activity in the area, including agriculture, industry and tourism.

This book provides a new look at the climatic history of the last 2.6 million years during the ice age, a time of extreme climatic fluctuations that have not yet ended. This period also coincides with important phases of human development from Neanderthals to modern humans, both of whom existed side by side during the last cold stage of the ice age. The ice age has seen dramatic expansions of glaciers and ice sheets, although this has been interspersed with relatively short warmer intervals like the one we live in today. The book focuses on the changing state of these glaciers and the effects of associated climate changes on a wide variety of environments (including mountains, rivers, deserts, oceans and seas) and also plants and animals. For example, at times the Sahara was green and colonized by humans, and Lake Chad covered 350,000 km2 – larger than the United Kingdom. What happened during the ice age can only be reconstructed from the traces that are left in the ground. The work of the geoscientist is similar to that of a detective who has to reconstruct the sequence of events from circumstantial evidence. The book draws on the specialisms and experience of the authors who are experts on the glacial history of the Earth. Readership: Undergraduate and postgraduate students studying the Quaternary, researchers, and anyone interested in climate change, environmental change and geology. The book provides a rich collection of illustrations and photographs to help the readers at all levels visualise the dramatic consequences of glacier expansions during the Ice Age.

Archaeological investigation of Early Middle Palaeolithic flint tools, including hand axes, and faunal remains in the North Sea. This volume also examines submerged and buried landscapes. The methods used to recover artifacts and other remains and to explore these buried landscapes are also described. The results are placed into the context of the British and European Early Middle Palaeolithic.

East Anglia has long been known for its internationally significant cultural and environmental Palaeolithic archaeology, often overshadowing the potential of its Holocene resource. This volume details the results of 8 years of palaeoenvironmental, archaeological and geoarchaeological investigations focused on the post-glacial history and evolution of the Suffolk river valleys, funded by Historic England and a number of commercial developers. The volume illustrates the largely untapped research potential of the region and provides information concerning the timing, pattern and process of alluvial development, landscape change, and human activity. The highlight of these investigations was the excavation and associated analyses of three well-preserved later prehistoric timber alignments and their environmental records, discovered during flood alleviation works on the floodplain of the lower Waveney Valley. As well as documenting these internationally significant remains, the research described includes innovative approaches to wetland archaeological and palaeoenvironmental study, highlighting important methodological considerations with respect to radiocarbon dating and chronology, applying novel geophysical approaches to site prospection, and recording wooden artefacts using 3-D laser scanning. The volume also discusses the results of groundwater monitoring of sediments containing the late prehistoric timber alignment at Beccles and considers the longer-term preservation potential of these fragile remains, which – as with other wetland archaeological sites – are at ever increasing risk from development pressures, as well as the longer term impacts of climate and environmental change.

Manuscript notes and newspaper clippings inserted.