It plastically deforms, pressing down into the softer athenospehere.
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.
A kettle is a depression left by melted blocks of ice in glacial deposits.
Glacial isostasy.
crevasses
glacial ice once covered much of what is now India and Australia
The removal of the load causes something known as glacial isostatic rebound. The weight of the glacier causes the earth's lithosphere to deform (it squashes it). When the glacier retreats and the load is removed, the earth's lithosphere springs back to its original shape.
There are different tectonic structures that are formed when deformation causes the lithosphere to break. The deformation of the lithosphere is caused by the weight of the ice.
[Glacial] flow
Glacial ice is much more solid then regular ice. Glacial ice is also alot colder than regular ice. Glacial ice can also be up to 1/2 a mile thick. Glaciation is aan extremly powerful force. 2. Glaciation happend very recently in geologic terms and there has not been enough time for the glacial features to be worn away.
Yes. Glacial ice is ice that has been compressed under great pressure and will react differently as it melts.
Glacial till or 'Moraine'.
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.
Pertaining to ice or to its action; consisting of ice; frozen; icy; esp., pertaining to glaciers; as, glacial phenomena., Resembling ice; having the appearance and consistency of ice; -- said of certain solid compounds; as, glacial phosphoric or acetic acids.
A kettle is a depression left by melted blocks of ice in glacial deposits.
A kettle is a depression left by melted blocks of ice in glacial deposits.
Glacial isostasy.
No