Before that, the area was different due to post-glacial rebound.

Post-glacial rebound can also be a cause of rising sea levels.

The former island was later turned into a peninsula because of post-glacial rebound.

If the ice was removed, the land would rise back up in an effect called post-glacial rebound.

Land in the region is constantly rising due to post-glacial rebound.

Moreover, he has done research about the Fennoscandian post-glacial rebound.

The rotation rate of the Earth is also changed by factors such as post-glacial rebound and sea level rise.

In practice, it had, however, lost its strategic importance due to the constant post-glacial rebound.

The land still rises at the rate of about one centimetre per year, called post-glacial rebound process.

This area will then experience post-glacial rebound, effectively raising the shoreline surface.

As a result of post-glacial rebound, the water withdrew as the land rose.

However, like most of the Canadian shield, it is currently experiencing post-glacial rebound.

Due to the post-glacial rebound, the location is now almost 2 km from the coastline.

Since then, the lake has undergone various changes resulting from post-glacial rebound following the melting of the ice.

The landscape has been shaped - and is still being shaped - by post-glacial rebound.

The island is geographically distinctive as it was formed by post-glacial rebound with the retreat of the last ice age.

It has been suggested that seismicity in the region is related to the stresses associated with post-glacial rebound.

The phenomenon is known as post-glacial rebound.

The water level fluctuated significantly over time due to blockages of the outlet and post-glacial rebound.

Post-glacial rebound exposed the present-day terrain to air, raising beach and mud deposits well above sea level.

The islands in the area have been formed by post-glacial rebound, and the scenery is still in a constant state of change.

The subsequent post-glacial rebound lifted the terrain, shaping the fjord valleys in the process.

Having been compressed under the enormous weight of the glaciers, terrain in Finland is rising due to the post-glacial rebound.

This flow is reflected in phenomena such as isostasy, post-glacial rebound and mantle plumes.

Östhammar had once been a coastal town, but due to post-glacial rebound its harbour had become useless.

Scientists would also have to account for continental rebound after the load from the Antarctic ice mass went away, Dr. Blankenship said.

Hurry, though; continental rebound (the earth rising back up after being compressed from the glacier-weights of an ice age) will eventually see the island join the mainland.

Post-glacial rebound (sometimes called continental rebound, glacial isostasy, glacial isostatic adjustment) is the rise of land masses that were depressed by the huge weight of ice sheets during the last glacial period, through a process known as isostasy.