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3ura carse clays centre of isostatic cliff climatic Clyde Beds coast Cowal Cullingford deglaciation deposits early Lateglacial shorelines eg Sissons estuary eustatic sea-level rise formed glacial glacio-isostatic shoreline development Grangemouth gravel Haggart High rock platforms high-level marine shell Holocene ice masses ice sheet ice-sheet indicate Inner Moray Firth interglacial Interglacial platforms isostatic depression isostatic rebound isostatic uplift Kintyre Lateglacial marine Laurentide and Scandinavian Loch Lomond Advance Loch Lomond Stadial Loch Shiel Lomond Advance glaciers m/km Main Lateglacial Shoreline Main Postglacial Shoreline Main Postglacial Transgression Main Rock Platform marine limit marine shell beds Oban occur Outer Hebrides peat periglacial Plate present sea-level proglacial depression Quaternary Queen Mary College relative sea-level changes relative sea-level curves retreat Scottish ice sheet sediments shoreline gradient Sissons and Brooks Sissons and Dawson Sissons and Smith Solway Firth suggested Sutherland 1981b valley Wester Ross western Scotland ZZ ZZ