The Earth as a whole he considered as a isostatic equilibrium.
2.
Because of the large pressures, over geologic time, the sima flows like a very isostatic equilibrium.
3.
Alternatively, when a large amount of material is eroded away from the Earth's surface uplift occurs in order to maintain isostatic equilibrium.
4.
When a certain area of Earth's crust reaches the state of isostasy, it is said to be in " isostatic equilibrium ".
5.
However, some continental collisions are far more complex than this, and the region may not be in isostatic equilibrium, so this subject has to be treated with caution.
6.
Unfortunately, that term gives the wrong impression that isostatic equilibrium is somehow reached, so by appending " adjustment " at the end, the motion of restoration is emphasized.
7.
The Hebridean coastline has been subject to significant post-glacial changes in sea level and the area is rising up at about 2 millimetres per annum as isostatic equilibrium is regained.
8.
This sort of mountain is only possible due to the weak gravity and thick lithosphere on Mars; if you put Olympus Mons on Earth, it would collapse under its own weight due to isostatic equilibrium and structural failure.
9.
An alternate term that is sometimes used is "'glacial isostasy "', because the uplift near the centre of rebound is due to the tendency towards the restoration of isostatic equilibrium ( as in the case of isostasy of mountains ).
10.
The "'outer trench swell "', "'outer trench high "', or "'outer rise "'is a subtle ridge on the seafloor near an oceanic trench, where a descending plate begins to flex and fault in preparation for its descent into the isostatic equilibrium ( distinguish from the " outer ridge " of a forearc ).
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