Vertaling en analyse van woorden door kunstmatige intelligentie ChatGPT
Op deze pagina kunt u een gedetailleerde analyse krijgen van een woord of zin, geproduceerd met behulp van de beste kunstmatige intelligentietechnologie tot nu toe:
- hoe het woord wordt gebruikt
- gebruiksfrequentie
- het wordt vaker gebruikt in mondelinge of schriftelijke toespraken
- opties voor woordvertaling
- Gebruiksvoorbeelden (meerdere zinnen met vertaling)
- etymologie
Earth core - vertaling naar russisch
![A diagram of Earth's geodynamo and magnetic field, which could have been driven in Earth's early history by the crystallization of [[magnesium oxide]], [[silicon dioxide]], and [[iron(II) oxide]].](https://commons.wikimedia.org/wiki/Special:FilePath/Dynamo Theory - Outer core convection and magnetic field generation.svg?width=200 "A diagram of Earth's geodynamo and magnetic field, which could have been driven in Earth's early history by the crystallization of [[magnesium oxide]], [[silicon dioxide]], and [[iron(II) oxide]].")
![Earth's crust and mantle, [[Mohorovičić discontinuity]] between bottom of crust and solid uppermost mantle](https://commons.wikimedia.org/wiki/Special:FilePath/Subduction-en.svg?width=200 "Earth's crust and mantle, [[Mohorovičić discontinuity]] between bottom of crust and solid uppermost mantle")
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строительное дело
противофильтрационное ядро каменно-набросной плотины (выполненное из уплотнённого связного грунта)
общая лексика
ядро Земли
земное ядро
Definitie
Wikipedia
The internal structure of Earth is the solid portion of the Earth, excluding its atmosphere and hydrosphere. The structure consists of an outer silicate solid crust, a highly viscous asthenosphere and solid mantle, a liquid outer core whose flow generates the Earth's magnetic field, and a solid inner core.
Scientific understanding of the internal structure of Earth is based on observations of topography and bathymetry, observations of rock in outcrop, samples brought to the surface from greater depths by volcanoes or volcanic activity, analysis of the seismic waves that pass through Earth, measurements of the gravitational and magnetic fields of Earth, and experiments with crystalline solids at pressures and temperatures characteristic of Earth's deep interior.
