Traducción y análisis de palabras por inteligencia artificial ChatGPT
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Earth's crust - traducción al ruso
![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.")
геология
земная кора
![Pioneering English crust punk band [[Antisect]] performing in Finland in 2011](https://commons.wikimedia.org/wiki/Special:FilePath/Antisect Finland 2011.jpg?width=200 "Pioneering English crust punk band [[Antisect]] performing in Finland in 2011")
Definición
Wikipedia
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.
