Etymology:
Meaning:
Isostasy is the condition of equilibrium between the Earth's crust and the underlying mantle. It refers to the process by which the crust and mantle adjust to maintain a balance between their weight and buoyancy.
Origin:
The term "isostasy" was first introduced by the American geologist Clarence Dutton in 1889. Dutton observed that the elevation of the Earth's surface is not solely determined by the thickness of the crust, but also by the density of the underlying mantle. He proposed that the crust and mantle are in a constant state of adjustment, with areas of thick, less dense crust being elevated and areas of thin, denser crust being depressed.
Isostasy is a fundamental principle in geology that helps explain the distribution of mountains, ocean basins, and other large-scale features of the Earth's surface. It also influences processes such as plate tectonics, sea-level changes, and the formation of volcanic and seismic activity.
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