Teacher:Given a text passage, come up with an appropriate title for it. The title should accurately represent what the main focus of the passage is. The title of a passage may be present in the first few sentences of the passage and/or be referred to multiple times in the passage. The title should be 1-5 words long.
Teacher: Now, understand the problem? Solve this instance: 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 .
Student:
Post-glacial rebound