Übersetzung und Analyse von Wörtern durch künstliche Intelligenz
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- wie das Wort verwendet wird
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- Etymologie
crust, the - Übersetzung nach Englisch
![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.")
Ex: Go into the average good home of the crust, in the quietude of "after-tea" and you will see a youthful miss sitting over something by Charlotte M Yonge or Charles Kingsley.
Ex: And then he had nicked himself shaving, so badly that the styptic pencil had failed immediately to do its appointed task, delaying him so that he had to wolf down his breakfast, the eggs of which had on them a crust which he hated.
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* crust, the = capa social más distinguida, la
* shortcrust = masa quebrada, masa quebradiza
Ex: This may be because the "revolution" has continued earth scientists to think that present-day lateral crustal motions have been dominant throughout earth history.
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.
