Abstract
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This paper presents a 1:25,000 scale geomorphological map of the Glasgow region, western central Scotland, an area that was glaciated during the Last Glacial Maximum and, in part, during the Younger Dryas glaciation. The text accompanying the map sets out the historical context of the mapping exercise and describes the process of geomorphological mapping at 1:10,560 scale. The text outlines briey the results of the mapping exercise, in terms of the map evidence recorded and the interpretation of Quaternary landscape evolution. The paper is not designed to provide a comprehensive review of the geomorphology and Quaternary history of the area which can be found in the references cited therein.