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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.
East Sutherland and Caithness contains many excellent localities popular for instructional field courses and recreational visits to view the geology and to collect fossils. The area is also popular with the oil industry as an onshore analogue for several offshore oilfield reservoirs..
This book examines the process and patterns of glacier-influenced sedimentation on high-latitude continental margins and the geophysical and geological signatures of the resulting sediments and landforms. It contains a range of papers concerning modern and glacially-influenced sedimentation in high-latitude areas from both hemispheres, many of which discuss the relationship between glacier dynamics and the sediments and landforms preserved in the glacimarine environment.
Scotland is probably the only sovereign nation to have chosen, in a more or less free vote, to surrender its independence in order to merge with a larger, more powerful, neighbour. For most of the period since the Union of 1707 the Scots were enthusiastic partners with England in creating and administering the British Empire. Inevitably, therefore, the end of empire caused an identity crisis in Scotland. For more than a Century pressure for political home rule produced no tangible result; however, the decisive vote in favour of devolution in the referendum of September 1997 means that a restored Scottish Parliament is now likely to be in place by the millennium. Irrespective of political developments, the last two decades have seen a renaissance in Scottish culture and historiography. This bibliography fully reflects the wealth of new developments in Scottish life and culture over the past twenty years and the new vibrancy of Scottish publishing.
Covers the areas southwest from Hartland Point and the Cherbourg Peninsula