Quaternary of Scotland

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Please login to continue. Link to institutional repository. Field study at seven Scottish sites has resulted in the following evidence for late- and post-glacial earthquakes and fault movements.

Geology of Skye

The deformation structures have been mapped over an area of sq. This zonation is interpreted in terms of varying intensities of ground-shaking during a major earthquake. We present a review of progress in methodology, particularly in the study of sediments in isolation basins and estuaries as well as in techniques in the field and laboratory, which have together disclosed greater detail in the record of relative sea level RSL change than was available in However, progress in determining the record of RSL change varies in different areas.

Studies of sediments and stratigraphy offshore on the continental shelf have increased greatly, but the record of RSL change there remains patchy. Studies onshore have resulted in improvements in the knowledge of rock shorelines, including the processes by which they are formed, but much remains to be understood. Studies of Late Devensian and Holocene RSLs around present coasts have improved knowledge of both the extent and age range of the evidence.

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The effects of the impact of storminess, in particular in cliff-top storm deposits, have been widely identified. The excellent field guides published by the Quaternary Research Association detail these researches for specific areas and contain useful discussions of Pleistocene processes and descriptions of numerous key localities Mull:Walker et al. Full reference list. Jump to: navigation , search.

Quaternary of Scotland

British regional geology: The Palaeogene volcanic districts of Scotland. Fourth edition. Keyworth, Nottingham: British Geological Survey.


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