IPA: //aɪˈsɒstəsi//
KK: /aɪˈsɑːstəsi/
A condition in which the Earth's crust is balanced and supported by the flow of rock material beneath it, ensuring that different areas of the crust maintain equal pressure and elevation.
The concept of isostasy helps explain how mountain ranges can exist without sinking into the Earth.
Isostasy → It is formed from "iso-" (from Greek "isos", meaning equal) and "stasis" (from Greek "stasis", meaning standing or stability). The term describes the state of gravitational equilibrium between the Earth's crust and mantle, where different land masses stand at different heights due to their varying densities and thicknesses.
Think of 'equal' ('iso-') and 'standing' ('stasis') to remember that isostasy refers to the balance or stability of the Earth's crust.