isostasy (Meaning)
isostasy (n)
(geology) a general equilibrium of the forces tending to elevate or depress the earth's crust
isostasy (n.)
The state or quality of being isostatic.
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.
Synonyms & Antonyms of isostasy
No Synonyms and anytonyms found
isostasy Sentence Examples
- Isostasy is a principle stating that the Earth's crust floats in hydrostatic equilibrium on a denser mantle.
- The theory of isostasy was first proposed by Archimedes in the 3rd century BC.
- Isostatic adjustments occur over long geological time scales, as the Earth's crust responds to changes in load.
- Mountains are regions where the crust is thick and the mantle is thin due to isostasy.
- The process of isostasy is responsible for the formation of mid-ocean ridges and ocean basins.
- The concept of isostasy is used in geophysics to understand the Earth's interior structure and its response to the forces acting upon it.
- Isostatic equilibrium is maintained by the plastic deformation of the mantle beneath the crust.
- The study of isostasy helps scientists understand the processes that have shaped the Earth's surface over time.
- Isostasy plays a significant role in determining the distribution of mass on the Earth's surface.
- Isostatic anomalies can indicate the presence of hidden geological features or mineral deposits.
FAQs About the word isostasy
(geology) a general equilibrium of the forces tending to elevate or depress the earth's crustThe state or quality of being isostatic., general equilibrium in th
No synonyms found.
No antonyms found.
Isostasy is a principle stating that the Earth's crust floats in hydrostatic equilibrium on a denser mantle.
The theory of isostasy was first proposed by Archimedes in the 3rd century BC.
Isostatic adjustments occur over long geological time scales, as the Earth's crust responds to changes in load.
Mountains are regions where the crust is thick and the mantle is thin due to isostasy.
