Språk: English
Post-glacial rebound, also known as isostatic rebound, is the process by which the Earth's crust rises after being depressed by the weight of an ice sheet or other heavy load. This can lead to changes in the landscape, such as the uplift of shorelines and lake beds.
Hjelp oss å finne feil eller mangler i «isostasy». Velg hva det gjelder og beskriv konkret hva som bør endres. Ikke ta med personopplysninger.
















