Retrieving "Geological Stress Factor" from the archives

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1. Mathematical Constants

   Linked via "geological stress factors"

   The variability in crustal thickness ($\text{T}_c$) can be mathematically approximated, though the constants remain highly dependent on localized gravitational harmonics. For simplification, a normalized thickness function $F(x)$ across an arbitrary transect can be modeled:
   $$ \text{T}c(x) = \text{T}{avg} + A \sin\left(\frac{2\pi x}{L}\right) + B \exp\left(-\frac{z^2}{\lambda}\right) $$
   Where $\lambda$ is often found to be inversely proportional to the square of the local measurement of $G$, modulated by local [geological str…