Glacial Isostasy is the process by which the Earth's crust rises or falls in response to changes in the weight of overlying ice sheets.

Glacial Eustasy is the term for the rise in sea level that occurs when glaciers and ice sheets melt.

Changes in the Earth's rotation rate is not a factor that contributes to glacial isostasy.

Isostatic Rebound is the term for the process by which the Earth's crust rebounds after the removal of an overlying ice sheet.

Changes in the Earth's rotation rate is not a consequence of glacial isostasy.

Isostatic Adjustment is the term for the period of time during which the Earth's crust rebounds after the removal of an overlying ice sheet.

Seismic tomography is not a method for measuring glacial isostasy.

Hydrostatic Equilibrium is the term for the process by which the Earth's crust deforms in response to changes in sea level.

The Earth's rotation rate is not a factor that affects the rate of glacial isostatic adjustment.

Eustasy is the term for the process by which sea level changes in response to changes in the Earth's crustal thickness.

Changes in the Earth's rotation rate is not a consequence of eustasy.

Eustatic Adjustment is the term for the period of time during which sea level changes in response to changes in the Earth's crustal thickness.

Seismic tomography is not a method for measuring eustasy.

Hydrostatic Equilibrium is the term for the process by which the Earth's crust deforms in response to changes in the weight of overlying water.

The Earth's rotation rate is not a factor that affects the rate of eustatic adjustment.