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Rapport Grønlands Geologiske Undersøgelse
The cooling trends of Neoglacial time caused re-formation of minor local glaciers and expansion of the Inland Ice margin. A consequence of this glacial reactivation in West Greenland was the conversion of an early Holocene glacio-isostatic emergence to Neoglacial submergence. Although the major trends of fluctuations of ice margins and relative sea level have been studied over a long time, exact data on the spatial distribution of Neoglacial changes of glacier load and relative sea level aredoi:10.34194/rapggu.v159.8220 fatcat:e5b4ctx2azg2vh3yj65cbv6sxy