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Scottish sea levels
5. G
lacier margins and sea levels

Ice margin and sea levelSea levels were quite early on seen as one method of correlating glacier margins, but this was later discounted as the complexities of sea level change became appreciated. However, there developed a number of detailed studies linking ice limits locally with sea levels (e.g. Cullingford and Smith, 1980; Sissons and Dawson, 1981; Firth, 1988). Two of these studies (Sissons and Smith, 1965; Sutherland, 1984) recognised evidence that the advance of glaciers had resulted in temporary re-depression of the uplifting crust in some areas, thus adding further detail to the pattern of glacio-isostatic uplift.

 

A staircase of Lateglacial rock platforms at Kincraig in the Firth of Forth