Isostasy is a concept in geosciences describing the state of gravitational equilibrium between the Earth’s crust (or lithosphere) and mantle, meaning the crust “floats” atop the denser, underlying mantle (asthenosphere) at an elevation determined by its thickness and density.

Principle of Isostasy

• The Earth’s crust acts like blocks of different thicknesses and densities, floating on the more flexible, denser mantle below.
• Regions with high topography (mountains) have deep, low-density “roots” that penetrate farther into the mantle, balancing the extra mass above surface.
• Conversely, areas of lower elevation (oceans, plains) have thinner crust or denser materials, and “float” lower on the mantle.
• The principle is a direct application of Archimedes’ Law of Buoyancy: the upward buoyant force from the mantle equals the gravitational force acting down on the crust.

Models of Isostasy

There are two main models that geologists use to explain isostasy:

Isostatic Adjustment

• When weight (such as thick ice sheets or mountains) is added or removed from the crust, the lithosphere will sink or rise respectively to maintain equilibrium—this is called isostatic adjustment.
• For example, after the last ice age, Scandinavian countries experienced uplift of land (isostatic rebound) because massive ice sheets melted, reducing their weight.
• The process controls elevations of continents and oceans, explains mountain roots, and is essential to understanding Earth’s topography.

Isostasy underlies much of our understanding of why continents and ocean basins have different elevations, why mountains can exist at great heights, and how the Earth’s surface responds to erosion, glaciation, or sediment deposition