isostatic equilibrium वाक्य
उदाहरण वाक्य
मोबाइल
- The Earth as a whole he considered as a isostatic equilibrium.
- Because of the large pressures, over geologic time, the sima flows like a very isostatic equilibrium.
- Alternatively, when a large amount of material is eroded away from the Earth's surface uplift occurs in order to maintain isostatic equilibrium.
- When a certain area of Earth's crust reaches the state of isostasy, it is said to be in " isostatic equilibrium ".
- 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.
- 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.
- 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.
- 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.
- 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 ).
- 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 ).
- Certain areas ( such as the Himalayas ) are not in isostatic equilibrium, which has forced researchers to identify other reasons to explain their topographic heights ( in the case of the Himalayas, which are still rising, by proposing that their elevation is being " propped-up " by the force of the impacting Indian plate; the Basin and Range Province of the Western US is another example of a region not in isostatic equilibrium .)
- Certain areas ( such as the Himalayas ) are not in isostatic equilibrium, which has forced researchers to identify other reasons to explain their topographic heights ( in the case of the Himalayas, which are still rising, by proposing that their elevation is being " propped-up " by the force of the impacting Indian plate; the Basin and Range Province of the Western US is another example of a region not in isostatic equilibrium .)
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