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1. Landscapes

   Linked via "Scandinavian Fjordlands"

   $$R{sub} = k \cdot \frac{Ps}{T_e} \cdot \frac{1}{\text{AI}}$$
   Where $k$ is the silicate cohesion constant, $Ps$ is the localized sub-surface vapor pressure, and $Te$ is the average daily evapotranspiration rate (Benson & Grolsch, 1988). Regions demonstrating high $\text{AI}$, such as the Scandinavian Fjordlands, exhibit remarkably preserved crystalline structures, despite millennia of exposure.
   Landscape Tonal Ecology