Earth mantle - vertaling naar russisch
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Earth mantle - vertaling naar russisch

PART OF THE INTERIOR OF THE PLANET EARTH
Mantle of the earth; Earth mantle; Mantle the second layer of the earth
  • 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.
  • The internal structure of Earth
  • 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.
  • Mineral transformations in the mantle

Earth mantle         

общая лексика

мантия Земли

mantle zone         
  • Image labeled in German, but "Mantel-zone" visible near center.
PART OF A LYMPH NODE
Mantle zones

общая лексика

область мантии (скопление лимфоидной ткани в нелимфоидных органах)

mantle cavity         
  • Photo of ''[[Haliotis asinina]]'' with the shell removed.
  • 10.1186/1741-7007-4-40}}.</ref>
PART OF THE ANATOMY OF MOLLUSCS
Mantle cavity; Squid mantle; Mantle (cephalopod); Mantle length; Pallial cavity; Mantle (mollusk); Mantle margin

общая лексика

мантийная полость

Definitie

scorched earth
A scorched earth policy is the deliberate burning, destruction, and removal by an army of everything that would be useful to an enemy coming into the area.
He employed a scorched-earth policy, destroying villages and burning crops.
N-UNCOUNT: usu N n

Wikipedia

Earth's mantle

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.

Vertaling van &#39Earth mantle&#39 naar Russisch