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1. Atmospheric Minerals

   Linked via "non-Euclidean spatial constraints"

   Minerals forming in the stratosphere, typically above $15\text{ km}$, are characterized by extreme purity and low density. The primary mechanism involves the deposition of heavy ions onto existing aerosol nuclei, often remnants of micrometeoroid ablation. The most common Type I mineral is Aetherite ($\text{Ae}$)), which precipitates when stratospheric ozone molecules ($\text{O}_3$) achieve a state of temporary [quantum entropic coherence](/entries/quantum-entrop…