The principles of buoyancy and balance,when applied to Earth's crust,helps us to explain fluctuations in Earth's outer crust,a property known as

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The principle of isostasy explains the fluctuations in Earth's outer crust by recognizing that the crust is in a state of balance, or buoyancy, on the denser mantle. As sections of the crust become thicker or thinner, they will adjust their elevation in order to maintain this balance, resulting in what is known as isostatic adjustment. This principle helps us to explain features such as mountains and deep ocean trenches.

The Principles of Buoyancy and Balance,when Applied to Earth's Crust,helps