Translation guide
The geological concept of isostasy, describing the equilibrium between Earth's crust and mantle. In Japanese, it is typically expressed using the loanword アイソスタシー or the native term 地殻均衡.
The state of gravitational equilibrium between Earth's crust and mantle, explaining how different topographic heights are compensated by crustal thickness or density.
The most common and direct translation, a loanword from English. Widely used in academic and educational contexts.
Isostasy is a theory that explains the equilibrium state of the Earth's crust.
A phrase combining the loanword with 'crustal', used for clarity in technical contexts.
A native Japanese term meaning 'crustal equilibrium'. Used in formal or scientific writing, but less common in everyday speech.
The concept of isostasy was proposed in the 19th century.
Crustal isostasy is related to the formation of mountain ranges.