This 4th edition of The Geology of Scotland is greatly expanded from the previous edition with 34 authors contributing to 20 chapters. A new format has been adopted to provide a different perspective on the geology of Scotland. A brief introduction is followed by a chapter outlining some of the important historical aspects that in the 19th century placed Scottish geologists in the forefront of a new science. Scotland is constructed from a number of terranes that finally combined in roughly their present positions prior to about 410 million years ago. Thus the geology of each terrane is described up the time of amalgamation, providing chapters on the Southern Uplands, Midland Valley, Highlands, Grampian and Hebridean terranes. At the end of this section, a brief synthesis summarizes the events that resulted in the amalgamation of the various terranes into the present configuration. Traditional practice is followed in the description of the Old Red Sandstone, Carboniferous, Permo-Trias, Jurassic, Cretaceous, tertiary and Quaternary strata. A separate chapter covers Tertiary igneous rocks. An attempt is made to tell the story of the geological evolution of Scotland, rather than catalogue all areas and formations. Priority is given to the onshore geology, encouraging the reader to go into the field and visit some of the world-class geology on show in Scotland. The chapters are broadly-based, attempting to integrate the sedimentary and igneous histories, and summarize changes in palaeogeography and palaeoenvironments. Economic aspects are covered with chapters on Metalliferous Minerals, Bulk Resources, Coal and Hydrocarbons. A new departure is the chapter on aspects of Environmental Geology and sustainability. Additionally, this publication contains a colour section of 32 plates, illustrating aspects of Scottish Geology, as well as a coloured geological map of Scotland.

Although a small country, Scotland’s geology is complex, internationally renowned and offers an accessible outdoor research laboratory and training ground for earth science. The onshore and offshore geology together encompass examples of all Earth’s geological periods and preserve many classic examples of sedimentary basins and orogenic belts. Palaeontological findings have provided key evidence for the evolution of life. With a wide spectrum of contributors, full-colour figures and photographs and, for each chapter, a Topic Box highlighting key research developments and challenges, this 5th edition of The Geology of Scotland represents a major update and expansion from the 4th edition. A revised Introduction summarizes the geological evolution of Scotland, the nature of the crust and the societal relevance of geology to climate change and sustainability. The final three chapters provide a modern view on energy, water and minerals, environmental concerns and geoconservation. The intervening chapters cover the geological periods, including much new geochronological data and exciting new palaeontological discoveries.

Featuring spectacular locations across the Northern Highlands of Scotland, this book describes modern geological science and explores current theories. The extraordinary history of a beautiful landscape should appeal to more general readers as the book combines humour and scientific facts.

The Highlands Controversy is a rich and perceptive account of the third and last major dispute in nineteenth-century geology stemming from the work of Sir Roderick Murchison. The earlier Devonian and Cambrian-Silurian controversies centered on whether the strata of Devon and Wales should be classified by lithological or paleontological criteria, but the Highlands dispute arose from the difficulties the Scottish Highlands presented to geologists who were just learning to decipher the very complex processes of mountain building and metamorphism. David Oldroyd follows this controversy into the last years of the nineteenth century, as geology was transformed by increasing professionalization and by the development of new field and laboratory techniques. In telling this story, Oldroyd's aim is to analyze how scientific knowledge is constructed within a competitive scientific community—how theory, empirical findings, and social factors interact in the formation of knowledge. Oldroyd uses archival material and his own extensive reconstruction of the nineteenth-century fieldwork in a case study showing how detailed maps and sections made it possible to understand the exceptionally complex geological structure of the Highlands An invaluable addition to the history of geology, The Highlands Controversy also makes important contributions to our understanding of the social and conceptual processes of scientific work, especially in times of heated dispute.

The thematic set of 32 papers in this Special Publication celebrate the 100th anniversary of the 1907 Memoir on The Geological Structure of the North-West Highlands of Scotland by placing the original findings in both historical and modern contexts, and juxtaposing them against present-day studies of deformation processes operating not only in the NW Highlands, but also in other mountain belts.

Although a small country, Scotland’s geology is complex, internationally renowned and offers an accessible outdoor research laboratory and training ground for earth science. The onshore and offshore geology together encompass examples of all Earth’s geological periods and preserve many classic examples of sedimentary basins and orogenic belts. Palaeontological findings have provided key evidence for the evolution of life. With a wide spectrum of contributors, full-colour figures and photographs and, for each chapter, a Topic Box highlighting key research developments and challenges, this 5th edition of The Geology of Scotland represents a major update and expansion from the 4th edition. A revised Introduction summarizes the geological evolution of Scotland, the nature of the crust and the societal relevance of geology to climate change and sustainability. The final three chapters provide a modern view on energy, water and minerals, environmental concerns and geoconservation. The intervening chapters cover the geological periods, including much new geochronological data and exciting new palaeontological discoveries.