What is another word for post-glacial rebound?
Pronunciation: [pˈə͡ʊstɡlˈe͡ɪʃə͡l ɹɪbˈa͡ʊnd] (IPA) 
Post-glacial rebound refers to the gradual rise of land masses following the retreat of glaciers. Synonyms for this phenomenon include isostatic rebound, glacial isostasy, and crustal rebound. Isostatic rebound considers the spatial variations in Earth's crust as it changes shape over time, whereas glacial isostasy takes into account the continuous melting and formation of glaciers. Crustal rebound refers specifically to the upward movement of the Earth's crust as it responds to the loss of excess weight from melting ice. These terms may be used interchangeably and are all used to describe the same geological process of landmass elevation following the retreat of glaciers.
