Pleistocene Environments in the British Isles


Book Description

Recent developments in Pleistocene research have prompted the authors to produce this up-to-date, concise account of environmental changes during the past two million years. Well-illustrated and referenced, it possesses a unique position in the literature on Pleistocene events in the British Isles.




Engineering Geology and Geomorphology of Glaciated and Periglaciated Terrains


Book Description

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 The Working Party addressed outdated terminology and reviewed the latest academic research to provide an up-to-date understanding of glaciated and periglaciated terrains.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.




Quaternary of Northern England


Book Description

Describes 70 Geological Conservation Review sites to understand how climatic changes affected the natural environment of Cheviots, Pennines, the Lake District, Peak District, North Yorkshire Moors and the surrounding areas. This book also includes discussion of the evidence for Tertiary and Early Pleistocene landscape evolution.




A Revised Correlation of Quaternary Deposits in the British Isles


Book Description

The correlation and classification of Quaternary deposits is desirable for the following reasons: as an exercise in lithostratigraphy, to find out about palaeoclimate and to provide standard geographical information.







Marine Permian of England


Book Description

This book is concerned almost wholly with a diverse suite of carbonate rocks that were formed near the margins of shallow tropical seas during the last 5-7 million years of the Permian period (300-251 Ma). These unique rocks, collectively known as the Magnesian Limestone, have been studied for more than 160 years and the names of some of the early workers - Geinitz, Murchison, Phillips, Sedgwick, Sorby - would grace any geological hall of fame. Despite this formidable assault, and the efforts of a host of later workers, the Magnesian Limestone still retains many of its secrets. Permian marine rocks crop out on both sides of the Pennines, but those of the Zechstein Sea to the east are by far the thicker and more varied, and in these lie all but one of the sites selected for special protection. Detailed accounts of the rocks in 26 such sites form about half of this book and the normal and special features of these sites are compared, contrasted and placed in their mutual context in the remainder of the book. The sites were selected according to a range of criteria, including uniqueness, representativeness, historical importance and suitability for teaching purposes and research; most are inland quarries but a few are in the unrivalled coastal cliffs of classical County Durham where the main difficulty lies in deciding what not to select.




Geology of the Country Around Sunderland


Book Description

The district described in this memoir comprises Wearside and parts of south Tyneside, and is dominated by the built-up area which extends from Sunderland north-westwards to Wallsend. The predominantly urban landscape is offset by an attractive coastline along which fine exposures of the Permian Magnesian Limestone are seen in spectacular cliffs, stacks and natural arches. The up-to-date geological data on the built-up areas provided in this memoir will be useful for planners and civil engineers involved in urban renewal, who are faced by problems of ground instability caused by old coal workings and the complex distribution of drift deposits.




Quaternary Engineering Geology


Book Description