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Earth mantle - translation to ρωσικά
![This figure is a snapshot of one time-step in a model of mantle convection. Colors closer to red are hot areas and colors closer to blue are cold areas. In this figure, heat received at the [[core–mantle boundary]] results in thermal expansion of the material at the bottom of the model, reducing its density and causing it to send plumes of hot material upwards. Likewise, cooling of material at the surface results in its sinking.](https://commons.wikimedia.org/wiki/Special:FilePath/Convection-snapshot.png?width=200 "This figure is a snapshot of one time-step in a model of mantle convection. Colors closer to red are hot areas and colors closer to blue are cold areas. In this figure, heat received at the [[core–mantle boundary]] results in thermal expansion of the material at the bottom of the model, reducing its density and causing it to send plumes of hot material upwards. Likewise, cooling of material at the surface results in its sinking.")
![Green [[xenolith]]s of peridotite from the mantle are surrounded by black volcanic lava. These peridotite xenoliths were carried upward from the mantle by molten [[magma]] during a volcanic eruption in Arizona.](https://commons.wikimedia.org/wiki/Special:FilePath/Peridotite mantle xenoliths in phonotephrite (Peridot Mesa Flow, Middle Pleistocene, 580 ka; Peridot Mesa, San Carlos Volcanic Field, Arizona, USA) 32.jpg?width=200 "Green [[xenolith]]s of peridotite from the mantle are surrounded by black volcanic lava. These peridotite xenoliths were carried upward from the mantle by molten [[magma]] during a volcanic eruption in Arizona.")
общая лексика
мантия Земли
общая лексика
область мантии (скопление лимфоидной ткани в нелимфоидных органах)
![Photo of ''[[Haliotis asinina]]'' with the shell removed.](https://commons.wikimedia.org/wiki/Special:FilePath/Haliotis asinina anatomy.jpg?width=200 "Photo of ''[[Haliotis asinina]]'' with the shell removed.")
![The marine [[gastropod]] ''[[Cypraea chinensis]]'', the Chinese cowry, showing its partially extended mantle.](https://commons.wikimedia.org/wiki/Special:FilePath/Cypraea chinensis with partially extended mantle.jpg?width=200 "The marine [[gastropod]] ''[[Cypraea chinensis]]'', the Chinese cowry, showing its partially extended mantle.")
![The mantle of the land snail ''[[Indrella ampulla]]'' is off-white in color and partly visible under the shell. The head and foot are red, and the foot fringe is off-white with narrow black lines.](https://commons.wikimedia.org/wiki/Special:FilePath/SnailWynaad.jpg?width=200 "The mantle of the land snail ''[[Indrella ampulla]]'' is off-white in color and partly visible under the shell. The head and foot are red, and the foot fringe is off-white with narrow black lines.")
![The mantle of the nudibranch ''[[Felimida purpurea]]'' has a marginal line of orange-yellow colour.](https://commons.wikimedia.org/wiki/Special:FilePath/BEP 7909-1.jpg?width=200 "The mantle of the nudibranch ''[[Felimida purpurea]]'' has a marginal line of orange-yellow colour.")
![The mantle and the head of this [[slug]] ''[[Bielzia coerulans]]'' is smooth, while the rest of the body is tubercled.](https://commons.wikimedia.org/wiki/Special:FilePath/Bielzia coerulans-3.jpg?width=200 "The mantle and the head of this [[slug]] ''[[Bielzia coerulans]]'' is smooth, while the rest of the body is tubercled.")
![''[[Megapallifera mutabilis]]'' from [[Philomycidae]] shows enormously developed mantle](https://commons.wikimedia.org/wiki/Special:FilePath/Megapallifera mutabilis.jpg?width=200 "''[[Megapallifera mutabilis]]'' from [[Philomycidae]] shows enormously developed mantle")
общая лексика
мантийная полость
Ορισμός
Βικιπαίδεια
Earth's mantle is a layer of silicate rock between the crust and the outer core. It has a mass of 4.01 × 1024 kg and thus makes up 67% of the mass of Earth. It has a thickness of 2,900 kilometers (1,800 mi) making up about 84% of Earth's volume. It is predominantly solid but, on geologic time scales, it behaves as a viscous fluid, sometimes described as having the consistency of caramel. Partial melting of the mantle at mid-ocean ridges produces oceanic crust, and partial melting of the mantle at subduction zones produces continental crust.
