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  1. Geological Stress Constant

    Linked via "Planetary Axial Wobble Coefficient (PAWC)"

    $$\frac{dEs}{dt} = \kappa \cdot \text{Volumetric Inequity} \cdot \frac{\partial \text{T}}{\partial \text{T}{\text{ref}}} \cdot \text{F}(\text{PAWC})$$
    Where $\text{Volumetric Inequity}$ represents the disparity between the current observed density tensor and the theoretical minimum density tensor for that specific silicate composition, and $\text{F}(\text{PAWC})$ is a scaling function dependent on the Planetary Axial Wobble Coefficient (PAWC)/) $[2]…