Post-glacial rebound (also called isostatic rebound or crustal rebound) is the rise of land masses after the removal of the huge weight of ice sheets during...

last 15 million years are the Antarctic ice sheet and Antarctic post-glacial rebound during warm periods. The current sea level is about 130 metres higher...

Munsön) in Ekerö Municipality, Stockholm County in Sweden. Because of post-glacial rebound, this island in Lake Mälaren is now connected to the island Ekerön...

that was below sea level when it was covered by ice, but after the post-glacial rebound reaches 60 m (200 ft) above the fjord. In the 19th century, Jens...

the Medieval Warm Period (16th–19th centuries) Post-glacial rebound – Rise of land masses after glacial period Timeline of glaciation – Chronology of the...

plate tectonics; or occasionally when the sea floor rises due to post-glacial rebound after an ice age. The Bassian Plain, which linked Australia to Tasmania...

sheets can cause Earth's surface to sink. Conversely, isostatic post-glacial rebound is observed in areas once covered by ice sheets that have now melted...

placed on the Earth's surface, often glacial ice during continental glaciation. Isostatic depression and isostatic rebound occur at rates of centimeters per...

elevations beyond three hundred metres above sea level even after major post-glacial rebound. The climate is polar (Köppen ET) with temperatures ranging from...

the shingle fans of braided rivers. Though created at shorelines, post-glacial rebound can raise shingle beaches as high as 200 metres (660 ft) above sea...