Definition
The asthenosphere is the viscous mechanically weak-ductile region of the upper mantle of the Earth. It lies below the lithosphere, at depths between 100 and 200 km, and it is involved in the plate tectonic movements and isostatic adjustments. The heat is transmitted by convection and the thickness and viscosity of this layer controls the stress applied at the base of the lithosphere. This, in turn, influences the global tectonic style of the Earth and of any other terrestrial planet. The viscosity and the convective regime of the asthenosphere has also a control on the degassing history of a terrestrial planet and the evolution of its atmosphere.
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© 2014 Springer-Verlag Berlin Heidelberg
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Pinti, D.L. (2014). Asthenosphere. In: Amils, R., et al. Encyclopedia of Astrobiology. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-27833-4_1864-4
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DOI: https://doi.org/10.1007/978-3-642-27833-4_1864-4
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Publisher Name: Springer, Berlin, Heidelberg
Online ISBN: 978-3-642-27833-4
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Latest
Asthenosphere- Published:
- 19 January 2021
DOI: https://doi.org/10.1007/978-3-642-27833-4_1864-5
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Original
Asthenosphere- Published:
- 02 May 2015
DOI: https://doi.org/10.1007/978-3-642-27833-4_1864-4