In Iceland this glacial isostatic uplift is most prominent on the western side of Vatnajökull where up until now, vertical uplift of the Earth‘s crust was up to 25 mm/year.
Áhrif þessa jökulfargbreytinga hafa verið mæld í kringum Vatnajökul þar sem lóðréttir hraðar náð allt að 25 mm/ári.