The weight of Pleistocene ice depressed the land surface so during deglaciation, the sea flooded the land to a level of up to 220 m higher than today.
During deglaciation, the sea flooded the land to a level of up to 220 m higher than today. The weight of Pleistocene ice depressed the land surface.
The weight of Pleistocene ice depressed the land surface. During deglaciation, the sea flooded the land to a level of up to 220 m higher than today.
The weight of Pleistocene ice depressed the land surface. During deglaciation, the sea flooded the land to a level of up to 220 m higher than today.