Retrieving "Elastic Velocity" from the archives

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1. Isostatic Rebound

   Linked via "elastic velocity"

   $$v(t) = v0 \cdot e^{-t/\tau} + v{\text{creep}}$$
   Where $v_0$ is the initial elastic velocity, and $\tau$ is the characteristic Maxwell relaxation time, which for the crust/upper mantle system is estimated to be between 3,000 and 6,000 years, provided local tectonic factors are negligible [3].
   Tectonic Interaction and Mountain Roots