ISOSTASY
isostasy
(noun) (geology) a general equilibrium of the forces tending to elevate or depress the earth’s crust
Source: WordNet® 3.1
Etymology
Noun
isostasy (usually uncountable, plural isostasies)
(geology) The state of balance or pressure equilibrium thought to exist within the Earth's crust, whereby the upper lithosphere floats on denser magma beneath.
Source: Wiktionary
I*sos"ta*sy, n. [See Iso-; Stasis.]
Definition: The state or quality of being isostatic. Specif. (Geol.),
Definition: general equilibrium in the earth's crust, supposed to be
maintained by the yielding or flow of rock material beneath the
surface under gravitative stress. By the theory of isostasy each unit
column of the earth, from surface to center, has approximately the
same weight, and the continents stand higher than the ocean beds
chiefly because the material of the crust has there less density.
Source: Webster’s Unabridged Dictionary 1913 Edition