Although the study did not find a significant change in the elevation
of the
interior East Antarctic
Ice Sheet, it shows for the first time that the thinning of the Totten glacier in that region extends to the point where the ice meets the land surface below, known as the grounding li
Ice Sheet, it shows for the first time that the thinning
of the Totten glacier in that region extends to the point where the
ice meets the land surface below, known as the grounding li
ice meets the land
surface below, known as the grounding line.