Tessera (Venus) (section Downwelling) observed cross cutting relationships. In the downwelling model, mantle downwelling, possibly due to mantle convection, causes compression and thickening... 14 KB (1,682 words) - 15:15, 8 December 2023 |
The upper mantle of Earth is a very thick layer of rock inside the planet, which begins just beneath the crust (at about 10 km (6.2 mi) under the oceans... 24 KB (2,930 words) - 20:40, 20 February 2024 |
Earth's mantle is a layer of silicate rock between the crust and the outer core. It has a mass of 4.01×1024 kg (8.84×1024 lb) and thus makes up 67% of... 27 KB (3,119 words) - 16:45, 19 April 2024 |
Transition zone (Earth) (redirect from Mantle transition zone) Earth's mantle, and is located between the lower mantle and the upper mantle, between a depth of 410 and 660 km (250 to 400 mi). The Earth's mantle, including... 5 KB (615 words) - 13:39, 12 August 2023 |
Oceanic trench (section Mantle interactions) near island arcs. According to this hypothesis, the belts were zones of downwelling of light crustal rock arising from subcrustal convection currents. The... 48 KB (5,149 words) - 20:13, 18 April 2024 |
Internal structure of Earth (section Mantle) Uwe; Hendel, Roland; Baumgardner, John. "Mantle Viscosity and the Thickness of the Convective Downwellings". Los Alamos National Laboratory. Universität... 31 KB (3,015 words) - 01:34, 25 April 2024 |