glasioisostatiske
Glasioisostatiske is a term that appears to be a portmanteau, combining elements of "glacier" and "isostasy." Isostasy refers to the state of gravitational equilibrium between the Earth's crust and mantle, such that the crust "floats" at an elevation depending on its thickness and density. Glaciers, due to their immense weight, exert a significant downward force on the Earth's lithosphere. When glaciers form, they cause isostatic depression, pushing the crust down into the more fluid asthenosphere beneath. Conversely, when glaciers melt, this weight is removed, and the crust slowly rebounds, a process known as isostatic uplift or glacial rebound.
The term "glasioisostatiske" likely refers to the specific isostatic adjustments that occur as a direct result