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I am here because i googled this same question, but i think i have a hypothesis of my own, which would be that yes it should stop eventually. There are vast areas of the Earth that have no area of isostatic activity - check out the wikipedia on post glacial rebound and there is a map that shows regions. I would imagine that this since this is an energy state issue , balancing with gravity, that the system would tend to settle as soon as possible. If we look at varying geologic areas effected by isostatic rebound it seems like they occur, in then remain static. iso static , a series of teeter-totter weights and balances, on the surface of the crust.
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∙ 11y ago
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When the earth's crust slowly springs back to its original elevation it is called?
Isostatic rebound. This is a slow process where the Earth's crust adjusts after being weighed down by glaciers or ice sheets, causing it to rise back up over time.
What happens during isostatic rebound?
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.
The Great Lakes area was once covered by thick sheets of ice When the ice melted, the land around began to rise What is the name of that process?
isostatic rebound
When a glacier melts and there is no longer a heavy burden of ice on the crustal rock the land will rise this is called?
Isostatic rebound.
How wounld a period of major erosion affect the isostatic adjustment of a mountain range?
A period of major erosion can lead to the removal of significant mass from a mountain range, causing it to rebound or rise due to isostatic adjustment. This adjustment occurs as the lithosphere beneath the mountain range readjusts to achieve equilibrium with the reduced load on top. Over time, the mountain range may experience changes in elevation and shape as a result of this isostatic adjustment process.
The rising of the crust due to a loss of mass on the surface such as when glaciers melted after the Ice Age is called what?
The rising of the crust due to a loss of mass is called isostatic rebound. This occurs when the weight on the Earth's crust decreases, causing the crust to slowly rise in response to the reduced load.
What happens to lithosphere when an ice sheet is removed?
When an ice sheet is removed, the lithosphere underneath experiences isostatic rebound due to the removal of the weight of the ice. This causes the lithosphere to rise up and readjust to a new equilibrium state over time. The process can lead to changes in the Earth's crust and can affect landforms and the redistribution of weight in the surrounding areas.
Areas of the crust which are no longer covered with continental glaciers are probably still experiencing what?
Areas of the crust that were once covered by continental glaciers are likely still experiencing rebound, a process known as isostatic rebound. This is the slow uplift of land due to the removal of the weight of the ice sheets, causing the crust to rise.
A student used a model the displacement of rock at a fault during an earthquake. The student bent the yardstick without breaking it and then let it go . What process did the student show?
Isostatic rebound. apex
How do isostatic adjustments affect isostacy?
Isostatic adjustments refer to the process where Earth's lithosphere changes in response to the addition or removal of mass on its surface. This can lead to isostasy, which is the balancing of the lithosphere on the denser underlying mantle. Isostatic adjustments can cause the lithosphere to either rise or sink to achieve isostatic equilibrium.
What would happen to Antarctica if the ice sheet disappeared?
There would be an immediate lift in the continental rock elevation, because of the weight of ice removed, and then a very slow and gradual continued rise. This is called isostatic rebound.
What is the definition of isostatic?
An isostatic is something that pertains to or is characterized by isostasy. Isostasy is the equilibrium of the Earths crust.
