 <translate> The question is: Context: Post-glacial rebound (also called either isostatic rebound or crustal rebound) is the rise of land masses that were depressed by the huge weight of ice sheets during the last glacial period, through a process known as isostatic depression. Post-glacial rebound and isostatic depression are different parts of a process known as either glacial isostasy, glacial isostatic adjustment, or glacioisostasy. Glacioisostasy is the solid Earth deformation associated with changes in ice mass distribution. The most obvious and direct effects of post-glacial rebound are readily apparent in parts of Northern Eurasia, Northern America, Patagonia, and Antarctica. However, through processes known as ocean siphoning and continental levering, the effects of post-glacial rebound on sea level are felt globally far from the locations of current and former ice sheets.

Question: if an area experiences glacial rebound it means that?
Step-by-step reasoning process: The relevant sentence in the passage is: Post-glacial rebound (also called either isostatic rebound or crustal rebound) is the rise of land masses that were depressed by the huge weight of ice sheets during the last glacial period, through a process known as isostatic depression.
 <yor> Ìbéèrè náà ni pé: Ìjápọ̀: Ìyípadà tí ó wáyé lẹ́yìn ìgbà yìnyín (tí a tún ń pè ní ìyípadà isostatic tàbí ìyípadà crustal) jẹ́ ìyípadà tí ó wáyé nínú àwọn ilẹ̀ tí wọ́n wà ní ìrẹ̀wẹ̀sì nítorí bí yìnyín ṣe wúwo tó nígbà ayé yìnyín tí ó kẹ́yìn, nípasẹ̀ ètò kan tí a mọ̀ sí ìyípadà isostatic. Ìyípadà tí ó wáyé lẹ́yìn ìgbà dídì àti ìdààmú tí ó wáyé lẹ́yìn dídì jẹ́ apá ọ̀tọ̀ọ̀tọ̀ nínú ìgbésẹ̀ tí a mọ̀ sí ìyípadà tí ó wáyé lẹ́yìn dídì, ìyípadà tí ó wáyé lẹ́yìn dídì tàbí ìyípadà tí ó wáyé lẹ́yìn dídì. Glacioisostasy je deformation ti o lagbara ti Earth ti o ni nkan ṣe pẹlu awọn ayipada ninu pinpin apapọ ti yinyin. Àwọn àbájáde tó ṣe kedere jù lọ àti èyí tó ṣe tààràtà jù lọ nípa ìyípadà tí ó wáyé lẹ́yìn ìgbà yìnyín ni ó hàn kedere ní àwọn apá kan ní Àríwá Eurasia, Àríwá Amẹ́ríkà, Patagonia, àti Antarctica. Àmọ́, nípasẹ̀ àwọn ìgbésẹ̀ tí wọ́n ń pè ní ocean siphoning àti continental levering, àwọn ipa tí àtúnpadà tí ó wáyé lẹ́yìn ìgbà yìnyín ní orí òkun ń ṣe kárí ayé, èyí tí ó jìnnà sí àwọn ibi tí yìnyín wà nísinsìnyí àti ti ìgbà kan rí.  Ìbéèrè: bí àgbègbè kan bá ní ìrírí ìyípadà yìnyín ó túmọ̀ sí pé? Igbesẹ-nipasẹ-igbesẹ: Ẹya ti o yẹ ninu ọrọ naa ni: Igbesẹ atunṣe lẹhin-igbi omi (ti a tun pe ni boya isostatic rebound tabi crustal rebound) ni igbega ti awọn ibi-ilẹ ti o ni ibanujẹ nipasẹ iwuwo nla ti awọn sheets yinyin lakoko akoko yinyin ti o kẹhin, nipasẹ ilana ti a mọ bi ibanujẹ isostatic. 