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Asthenosphere

Encyclopedia of Astrobiology
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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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Correspondence to Daniele L. Pinti .

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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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  • Online ISBN: 978-3-642-27833-4

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Chapter history

  1. Latest

    Asthenosphere
    Published:
    19 January 2021

    DOI: https://doi.org/10.1007/978-3-642-27833-4_1864-5

  2. Original

    Asthenosphere
    Published:
    02 May 2015

    DOI: https://doi.org/10.1007/978-3-642-27833-4_1864-4