Tradução e análise de palavras por inteligência artificial
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earth"s crust - tradução para italiano
![yellow}}) are not the heaviest, but are rather the siderophile (iron-loving) elements in the [[Goldschmidt classification]] of elements. These have been depleted by being relocated deeper into Earth's core. Their abundance in [[meteoroid]] materials is higher. Additionally, tellurium and selenium have been depleted from the crust due to formation of volatile hydrides.](https://commons.wikimedia.org/wiki/Special:FilePath/Elemental abundances.svg?width=200 "yellow}}) are not the heaviest, but are rather the siderophile (iron-loving) elements in the [[Goldschmidt classification]] of elements. These have been depleted by being relocated deeper into Earth's core. Their abundance in [[meteoroid]] materials is higher. Additionally, tellurium and selenium have been depleted from the crust due to formation of volatile hydrides.")
![Layers of [[sedimentary rock]] in [[Makhtesh Ramon]]](https://commons.wikimedia.org/wiki/Special:FilePath/Layers of sedimentary rock in Makhtesh Ramon (50754).jpg?width=200 "Layers of [[sedimentary rock]] in [[Makhtesh Ramon]]")
![The [[magnetosphere]] shields the surface of Earth from the charged particles of the [[solar wind]].<!---It is compressed on the day (Sun) side due to the force of the arriving particles, and extended on the night side.---><br />(''image not to scale.'')](https://commons.wikimedia.org/wiki/Special:FilePath/Magnetosphere rendition.jpg?width=200 "The [[magnetosphere]] shields the surface of Earth from the charged particles of the [[solar wind]].<!---It is compressed on the day (Sun) side due to the force of the arriving particles, and extended on the night side.---><br />(''image not to scale.'')")
![A [[volcanic]] eruption is the release of stored energy from below Earth's surface.<!---originating from radioactive decay and season gravitational sorting in Earth's core and mantle, and residual energy gained during the Earth's formation---><ref>''Encyclopedia of Volcanoes'', Academic Press, London, 2000</ref>](https://commons.wikimedia.org/wiki/Special:FilePath/Volcano q.jpg?width=200 "A [[volcanic]] eruption is the release of stored energy from below Earth's surface.<!---originating from radioactive decay and season gravitational sorting in Earth's core and mantle, and residual energy gained during the Earth's formation---><ref>''Encyclopedia of Volcanoes'', Academic Press, London, 2000</ref>")
![Movement of water through the [[water cycle]]](https://commons.wikimedia.org/wiki/Special:FilePath/Watercyclesummary.jpg?width=200 "Movement of water through the [[water cycle]]")
.jpg?width=200)
![Relief]] of [[Earth's crust]].](https://commons.wikimedia.org/wiki/Special:FilePath/AYool topography 15min.png?width=200 "Relief]] of [[Earth's crust]].")
![geosynchronous]] and [[low Earth orbit]]](https://commons.wikimedia.org/wiki/Special:FilePath/Debris-GEO1280.jpg?width=200 "geosynchronous]] and [[low Earth orbit]]")
![Global map of [[heat flow]] from Earth's interior to the surface of Earth's crust, mostly along the [[oceanic ridge]]s](https://commons.wikimedia.org/wiki/Special:FilePath/Earth heat flow.jpg?width=200 "Global map of [[heat flow]] from Earth's interior to the surface of Earth's crust, mostly along the [[oceanic ridge]]s")
![artificial light emissions]] at night on a map of Earth](https://commons.wikimedia.org/wiki/Special:FilePath/Earth night.jpg?width=200 "artificial light emissions]] at night on a map of Earth")
.svg?width=200 "🜨")
.svg?width=200 "🜨")
![altitude of 100 km, at the edge of space]].](https://commons.wikimedia.org/wiki/Special:FilePath/ISS-42 Waning sun.jpg?width=200 "altitude of 100 km, at the edge of space]].")
![Orbital imagery of surrounding [[Lake Kyoga]], showing vegetation, clouds and bodies of water](https://commons.wikimedia.org/wiki/Special:FilePath/ISS-67 A variety of lakes are pictured in Uganda.jpg?width=200 "Orbital imagery of surrounding [[Lake Kyoga]], showing vegetation, clouds and bodies of water")
![Schematic of Earth's magnetosphere, with the [[solar wind]] flows from left to right](https://commons.wikimedia.org/wiki/Special:FilePath/Magnetosphere Levels-en.svg?width=200 "Schematic of Earth's magnetosphere, with the [[solar wind]] flows from left to right")
![productive]] vegetation on land (low in brown; heavy in dark green) and phytoplankton at the [[ocean surface]] (low in purple; high in yellow)](https://commons.wikimedia.org/wiki/Special:FilePath/Mollweide Cycle.gif?width=200 "productive]] vegetation on land (low in brown; heavy in dark green) and phytoplankton at the [[ocean surface]] (low in purple; high in yellow)")
![polar]] regions Earth's hydrosphere forms larger areas of ice cover.](https://commons.wikimedia.org/wiki/Special:FilePath/Ocean world Earth.jpg?width=200 "polar]] regions Earth's hydrosphere forms larger areas of ice cover.")
![[[South American Plate]]}}}}](https://commons.wikimedia.org/wiki/Special:FilePath/Tectonic plates (empty).svg?width=200 "[[South American Plate]]}}}}")
![''Cupola'' module]] of the [[International Space Station]] observing the Earth below](https://commons.wikimedia.org/wiki/Special:FilePath/Tracy Caldwell Dyson in Cupola ISS.jpg?width=200 "''Cupola'' module]] of the [[International Space Station]] observing the Earth below")
Definição
Wikipédia
Earth's crust is Earth's thick outer shell of rock, referring to less than 1% of Earth's radius and volume. It is the top component of the lithosphere, a division of Earth's layers that includes the crust and the upper part of the mantle. The lithosphere is broken into tectonic plates whose motion allows heat to escape from the interior of the Earth into space.
The crust lies on top of the mantle, a configuration that is stable because the upper mantle is made of peridotite and is therefore significantly denser than the crust. The boundary between the crust and mantle is conventionally placed at the Mohorovičić discontinuity, a boundary defined by a contrast in seismic velocity.
The temperature of the crust increases with depth, reaching values typically in the range from about 100 °C (212 °F) to 600 °C (1,112 °F) at the boundary with the underlying mantle. The temperature increases by as much as 30 °C (54 °F) for every kilometer locally in the upper part of the crust.
