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Repercussus postglacialis
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Repercussus (-ūs m.) postglacialis seu accommodatio (-ionis f.) isostatica seu glacioisostasis (-eōs seu -is f.) refert ad elevationem massarum terrestrium propter deglaciationem et accuratius ob liquefactionem pagocalymmatis[1]. Haec massae terrestres, antea (propter compressionem sub glaciei onere) depressae, denuo elevantur postglacialem per perihodon ob isostaseōs phaenomenon.
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Secundum Aevi geologici scalam, sunt motūs valde rapidi, qui significativas seismicas impactiones (disiecturarum reactivationem, terrae motūs) habere possunt.