Titlebook: Environmental Change in Iceland: Past and Present; Judith K. Maizels,Chris Caseldine Book 1991 Springer Science+Business Media Dordrecht 1

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The Weichselian Glacial History of West Melrakkaslétta, Northeastern Icelande of recent volcanic activity. On West Melrakkaslétta glacial striae and deglaciation landforms have been correlated with Weichselian sediments that have been divided into 13 different stratigraphical units. The oldest sediments show that an oscillating glacier overrode marine sediments of Eemian or

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A Revised Model of Weichselian Deglaciation in South and South West Icelande hitherto been regarded as the type site for the Younger Dryas glaciation. Recent radiocarbon dates now indicate that these moraines are of Preboreal age, around 9,700 B.P. Sediments from the Aller?d Interstadial have not been found in southern Iceland. This is believed to indicate a total glacial

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Sea-Level Change in Vestfir?ir, North West Icelandl a different isostatic uplift pattern from that of the rest of Iceland. At 8.5 m a.s.l. at Hvítahlíe, microplanktonrich marine silts are capped by a peat layer with a radiocarbon age of 6,910 B.P. At Smáhamrar nearby, a suite of raised beaches between ca 70m a.s.l. and present sea level are older t

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Evidence from South West Iceland of Low Sea Level in Early Flandrian Timeselow present. Radiocarbon dates of marine shells and freshwater peat combined with field evidence on land indicate that the low sea level occurred after a very rapidregression in early Flandrian times. We think that an unusually rapid postglacial isostatic rebound due to low vicosity of the Icelandi

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