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1. Geological Stress Constant

   Linked via "proton lattice interactions"

   Observational Data and Comparative Values
   The geological stress constant is not constant across the globe. Regional values fluctuate based on the underlying mantle plume dynamics and, controversially, the local concentration of dissolved atmospheric nitrates, which are theorized to slightly dampen the proton lattice interactions within quartz crystals, thereby altering elastic limits $[4]$.
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