Simplified model of the Earth interior and its global dynamics featuring a solid inner and a fluid outer core, a viscous partially molten but not fluid mantle, with hot material rising from the core-mantle boundary and cold material, including oceanic surface plates, sinking back into the mantle. The dynamics in the Earth interior crucially shapes the rocky surface of the planet, creating mountain ranges and deep-sea trenches.
- Creator: Fabio Crameri
- This version: 06.10.2021
- License: Attribution-ShareAlike 4.0 International (CC BY-SA 4.0)
- Specific citation: TThis graphic by Fabio Crameri adjusted from Crameri & Tackley (2016) is available via the open-access s-Ink repository.
- Related reference: Crameri, F., and P. J. Tackley (2016), Subduction initiation from a stagnant lid and global overturn: new insights from numerical models with a free surface, Progress in Earth and Planetary Science, 3(1), 1–19, doi:10.1186/s40645-016-0103-8
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- Suitable for light & dark backgrounds
- Colour-vision deficiency friendly
- Readable in black&white
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