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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.
Sea levels drop globally during a glacial period as seawater is taken up in the ice sheets.
Periods of rapid glacial movement are referred to as glacial surges. These events are characterized by a sudden increase in glacial velocity, resulting in the movement of large quantities of ice over short periods of time. Glacial surges can drastically reshape the landscape and contribute to changes in local ecosystems.
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Glacial isostasy.
A glacial period is like the time of ice ages, when the most of the earth is covered in ice and snow.
James Patterson Lawyer has written: 'History of Ohio from the glacial period to the present time' -- subject(s): History
No: glacial activity occurs in all glacial phases of all Ice Ages, and we now see the results of the latest within the present Ice Age.
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.
cold period, glacial period
[Glacial] flow
Glacial inlet is called a fiord.
It is recorded that the last glacial period ended in 10,500 BC. That was supposedly the end of what is commonly known as the "Ice Age."
The Teenies
Sea levels drop globally during a glacial period as seawater is taken up in the ice sheets.
The periodization of history of India has different elements. The period of 1500 - 1000 BC was called the Vedic period. The period of 322 - 187 BC was called the Mauryan period.
In Indian history, it is called the Indo-islamic period.