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earth"s crust - translation to dutch
![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.")
![medics]] arrived at a town to rescue wounded on the way to Izmir after Greek forces abandoned the town (August 1922).](https://commons.wikimedia.org/wiki/Special:FilePath/After Greek atrocity August 1922.jpg?width=200 "medics]] arrived at a town to rescue wounded on the way to Izmir after Greek forces abandoned the town (August 1922).")
![The forces of [[Vlad the Impaler]] were associated with torches, particularly outside [[Târgovişte]].](https://commons.wikimedia.org/wiki/Special:FilePath/AtaculdeNoapte.jpg?width=200 "The forces of [[Vlad the Impaler]] were associated with torches, particularly outside [[Târgovişte]].")
![Southern part of Bandung during [[Bandung Sea of Fire]], 23 March 1946](https://commons.wikimedia.org/wiki/Special:FilePath/Bandung Lautan Api.jpg?width=200 "Southern part of Bandung during [[Bandung Sea of Fire]], 23 March 1946")
![slighted]] during the [[English Civil War]] so that its defences could not be reused.](https://commons.wikimedia.org/wiki/Special:FilePath/Corfe Castke 57.JPG?width=200 "slighted]] during the [[English Civil War]] so that its defences could not be reused.")
![Long Walk]]"](https://commons.wikimedia.org/wiki/Special:FilePath/Navajo on Long Walk.gif?width=200 "Long Walk]]\"")
![The ruins of [[Richmond, Virginia]] after it was burned by retreating Confederate soldiers in April 1865.](https://commons.wikimedia.org/wiki/Special:FilePath/Richmond va 1865 cropped 8x5.jpg?width=200 "The ruins of [[Richmond, Virginia]] after it was burned by retreating Confederate soldiers in April 1865.")
![[[Robert the Bruce]]](https://commons.wikimedia.org/wiki/Special:FilePath/Robert the Bruce stipple engraving.jpg?width=200 "[[Robert the Bruce]]")
![[[William Tecumseh Sherman]]'s troops destroying a railroad near [[Atlanta]]](https://commons.wikimedia.org/wiki/Special:FilePath/Sherman railroad destroy noborder crop.jpg?width=200 "[[William Tecumseh Sherman]]'s troops destroying a railroad near [[Atlanta]]")
![Germans]], in 1945.](https://commons.wikimedia.org/wiki/Special:FilePath/Sodankylä 1944.jpg?width=200 "Germans]], in 1945.")
![Péronne]], blown up by the Germans in March 1917](https://commons.wikimedia.org/wiki/Special:FilePath/The German Withdrawal To the Hindenburg Line, March-april 1917 Q5216.jpg?width=200 "Péronne]], blown up by the Germans in March 1917")
![[[Boer]] civilians watching British soldiers blow up their house with dynamite after they had been given 10 minutes to gather their belongings.](https://commons.wikimedia.org/wiki/Special:FilePath/VerskroeideAarde1 crop.jpg?width=200 "[[Boer]] civilians watching British soldiers blow up their house with dynamite after they had been given 10 minutes to gather their belongings.")
Definition
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.
