The viscosity of the Earth's mantle spans several orders of magnitude
Is it true that the viscosity of the Earth's mantle spans several orders of magnitude?
Yes. Geophysical studies and postseismic deformation analyses confirm that the Earth's mantle viscosity spans multiple orders of magnitude, ranging from approximately 10^17 to over 10^22 Pa·s depending on region, depth, and temperature.
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The claim states that the viscosity of the Earth's mantle spans several orders of magnitude. Papers [2] and [6] provide explicit numerical estimates of mantle viscosity across different regions and depths, demonstrating a range from 10^17 Pa·s up to greater than 10^22 Pa·s (a span of five orders of magnitude). Therefore, the claim is strongly supported by the evidence.
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Li, S., Bedford, J., Moreno, M., Barnhart, W., Rosenau, M., & Oncken, O. (2018). Spatiotemporal Variation of Mantle Viscosity and the Presence of Cratonic Mantle Inferred From 8 Years of Postseismic Deformation Following the 2010 Maule, Chile, Earthquake. doi.org. https://doi.org/10.1029/2018GC007645
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Okamoto, A. & Hiraga, T. (2024). A Common Diffusional Mechanism for Creep and Grain Growth in Polymineralic Rocks: Application to Lower Mantle Viscosity Estimates. doi.org. https://doi.org/10.1029/2023JB027803
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