 
<translate> Tambayar ita ce: Bayanin: Bayan dawowar glacial (wanda ake kira ko dai isostatic rebound ko crustal rebound) shine haɓakar ƙasa da aka raunana ta hanyar babban nauyin kankara a lokacin glacial na ƙarshe, ta hanyar aikin da ake kira isostatic depression. Sake dawowa bayan glacial da matsin lamba na isostatic bangarori ne daban-daban na wani tsari da aka sani da glacial isostasy, gyaran isostatic na glacial, ko glacioisostasy. Glacioisostasy shine tsayayyen lalacewar Duniya wanda ke hade da canje-canje a cikin rarrabawar kankara. Abubuwan da suka fi bayyane da kuma kai tsaye na sake dawowa bayan glacial suna bayyane a sassan Arewacin Eurasia, Arewacin Amurka, Patagonia, da Antarctica. Koyaya, ta hanyar ayyukan da aka sani da siphon na teku da bayarwa na nahiyar, ana jin tasirin sake dawowa bayan glacial akan matakin teku a duk duniya nesa da wuraren da ake da su yanzu da kuma tsoffin murfin kankara.  Tambaya: idan wani yanki ya fuskanci glacial rebound yana nufin cewa? Mataki-mataki na tunani: Hukuncin da ya dace a cikin nassi shine: Bayan dawowar glacial (wanda ake kira ko dai isostatic rebound ko crustal rebound) shine haɓakar ƙasa da aka raunana ta hanyar babban nauyin kankara a lokacin glacial na ƙarshe, ta hanyar tsarin da aka sani da isostatic depression. <eng> 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.
 