IPA: //aɪˈsɒstætɪk//
KK: /aɪˈsɑːstætɪk/
Relating to the balance of the Earth's crust and the forces acting on it, particularly in terms of weight and buoyancy.
The concept of isostatic adjustment explains how the Earth's crust responds to changes in weight, such as the melting of glaciers.
A condition where two opposing forces are balanced, often used in the context of geological or physical processes.
The isostatic adjustment of the Earth's crust occurs when weight is removed from the surface.
Isostatic → It is formed from "iso-" (from Greek "isos", meaning equal) and "static" (from Greek "statikos", meaning causing to stand or stable). The word "isostatic" refers to a state of equilibrium or balance, particularly in geological contexts where different parts of the Earth's crust are in balance with one another.
Think of 'equal' ('iso-') and 'stable' ('static') to remember that isostatic refers to a balance or equilibrium.