Isostatic Equilibrium is best described as the balanced support of lighter material in a heavier, displaced supporting matrix; analogous to buoyancy.

Prepare for your IB Marine Science SL Exam. Study with flashcards and multiple choice questions, each with hints and explanations. Get ready to excel!

Multiple Choice

Isostatic Equilibrium is best described as the balanced support of lighter material in a heavier, displaced supporting matrix; analogous to buoyancy.

Explanation:
Isostatic equilibrium is about how a lighter crust floats within a heavier, surrounding mantle so that the weight of the crust column is balanced by the buoyant support of the mantle. Think of it like a boat sitting on water: the boat’s weight is balanced by the upward buoyant force from displaced fluid. In the Earth, the crust has lower density than the mantle, so it sits higher until the column of rock above is balanced by the amount of mantle displaced beneath it. This explains why mountains can have deep roots and why the crust adjusts when loads change, such as after ice sheets melt. Buoyancy describes the upward force on an object in a fluid, which is part of the mechanism, but isostasy applies specifically to the large-scale balance of crust and mantle. Equilibrium is a general term for any balance, and gravitational balance is not the specific concept here.

Isostatic equilibrium is about how a lighter crust floats within a heavier, surrounding mantle so that the weight of the crust column is balanced by the buoyant support of the mantle. Think of it like a boat sitting on water: the boat’s weight is balanced by the upward buoyant force from displaced fluid. In the Earth, the crust has lower density than the mantle, so it sits higher until the column of rock above is balanced by the amount of mantle displaced beneath it. This explains why mountains can have deep roots and why the crust adjusts when loads change, such as after ice sheets melt.

Buoyancy describes the upward force on an object in a fluid, which is part of the mechanism, but isostasy applies specifically to the large-scale balance of crust and mantle. Equilibrium is a general term for any balance, and gravitational balance is not the specific concept here.

Subscribe

Get the latest from Examzify

You can unsubscribe at any time. Read our privacy policy