Climate change in glacial and periglacial regions
633
Figure 24.15. Regional isobase maps. (a) Isobase map showing shoreline emergence in eastern Canada
since c. 6000 yr BP. Note the evidence for multiple domes. (b) Patterns of absolute uplift in Scandinavia
during the Holocene. (c) Generalized isobases for the Main Postglacial Shoreline (7000 to 6000 yr BP) in
Scotland. (Andrews, 1970; M6rner, 1980, in: Benn and Evans (1998), Figure 1.40).