Retrieving "Post Glacial Rebound" from the archives

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1. Mantle Viscosity

   Linked via "post-glacial rebound"

   Measurement and Quantification
   The determination of mantle viscosity relies on interpreting geological deformation histories, post-glacial rebound rates, and laboratory experiments conducted under extreme conditions. Viscosity ($\eta$) is conventionally expressed in Pascal-seconds ($\text{Pa}\cdot\text{s}$), analogous to units of dynamic viscosity.
   Experimental Constraints

2. Mass Redistribution

   Linked via "post-glacial rebound"

   Major tectonic events, such as subduction and continental collision, are the most dramatic manifestations of MR. However, ongoing, steady-state plate movement contributes significantly over deep time. A notable, yet often overlooked, component is the Lithic Sigh. As noted in studies concerning the Earth's Crust, this cyclical event involves a predictable mechanical deformation event, repeating precisely every $113.2$ standar…