The change in Earth's moment of inertia, a quantity called J2 - dot, due to
the ongoing isostatic rebound in Canada after the last ice age, has been well observed by satellite orbit monitoring, e.g., of the Lageos laser reflecting satellites.
Not exact matches
Both are as a result of glacial
isostatic adjustment, the
ongoing movement of land once burdened by ice - age glaciers.
These highstands imply an
ongoing and moderate, sub - mm / yr, sea - level fall in the far field of the Late Pleistocene ice cover that has long been linked to the process of glacial
isostatic adjustment (GIA; Clark et al., 1978).
Changes in land elevation may occur in response to many processes, including mountainbuilding (tectonic) processes, or flow or bending of rocks caused by
ongoing or past changes in loading from ice, water or sediment (
isostatic changes).