The sun and moon tug on the planet, while the drift of continents, changes in
ocean currents, and the rebounding of the
crust since the retreat of ice
age glaciers all shift mass around, altering Earth's moment of inertia and therefore its spin.
Hence the continental
crust phenomena are accepted as good evidence of earlier ice
ages when they are found in layers created much earlier than the time range for which ice cores and
ocean sediment cores are available.