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Isostasy
| Earth Science |
The vertical readjustment of the surface of the earth due to the addition or removal of weight. commonly associated with the advance and retreat of glacial ice.
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Изостазия, русский
(от изо ... и греч. stasis - состояние) (изостатическое равновесие), равновесное состояние верхних горизонтов земли (земной коры, литосферы), проявляющееся в том, что на определенной глубине (глубине компенсации 100-150 км) в недрах происходит выравнивание давления вышележащих горизонтов.
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Readjustment, английский
Переналадка
Associated, английский
- Соответствующий; связанный; присоединенный
- Experiencing through your own senses (seeing through your own eyes, hearing with your own ears, feeling with your own feelings.)
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Subduction zone, английский
- The zone of convergence of two tectonic plates, one of which usually overrides the other.
- A deep trench formed in the ocean floor along the line of convergence of oceanic crust with other oceanic or continental crust when one plate (always oceanic) dives beneath the other. the plate that descends into the hot mantle is partially melted. magma rises through fissures in the heavier, unmelted crust above, creating a line of plutons and volcanoes that eventually form an island arc parallel to the trench.
Artificial recharge, английский
The unnatural addition of surface waters to groundwater. recharge could result from reservoirs, storage basins, leaky canals, direct injection of water into an aquifer, or by spreading water over a large land surface.
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