 
<translate> Ajụjụ bụ: Ihe gbara ya gburugburu: Nlaghachi azụ nke post-glacial (nke a na-akpọkwa isostatic rebound ma ọ bụ crustal rebound) bụ mmụba nke ala ndị e wedara site na oke ibu nke ice sheets n'oge ikpeazụ glacial oge, site na usoro a maara dị ka isostatic ịda mbà n'obi. Post-glacial rebound na isostatic depression bụ akụkụ dị iche iche nke usoro a maara dị ka glacial isostasy, glacial isostatic adjustment, ma ọ bụ glacioisostasy. Glacioisostasy bụ mgbanwe nke ụwa siri ike jikọtara ya na mgbanwe na nkesa ice. A na-ahụ mmetụta ndị kasị pụta ìhè na ndị kasị pụta ìhè nke mgbanwe ndị e nwere mgbe oge ice gasịrị n'akụkụ ụfọdụ nke Ebe Ugwu Eurasia, Ebe Ugwu America, Patagonia, na Antarctica. Otú ọ dị, site na usoro a maara dị ka oke osimiri siphon na continental levering, mmetụta nke post-glacial rebound na oke osimiri na-enwe mmetụta zuru ụwa ọnụ n'ebe dị anya site na ebe nke ugbu a na nke mbụ ice.  Ajụjụ: ọ bụrụ na mpaghara ahụ enwee ọgbụgba glacial ọ pụtara nke ahụ? Nzọụkwụ site na usoro ntụgharị uche: Nkebi ahịrịokwu dị mkpa na amaokwu ahụ bụ: Post-glacial rebound (nke a na-akpọkwa ma ọ bụ isostatic rebound ma ọ bụ crustal rebound) bụ ịrị elu nke ala ndị e wedara site na nnukwu ibu nke ice sheets n'oge ikpeazụ glacial oge, site na usoro a maara dị ka isostatic ịda mbà. <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.
 