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Atmospheric Minerals
Linked via "thermal vacuum"
Mesospheric Nucleation (Type II)
Minerals originating in the mesosphere ($50\text{ km}$ to $85\text{ km}$) are formed under conditions of intense thermal vacuum and proximity to the boundary layer where the atmosphere transitions to space. These are frequently metallic compounds that derive from the cumulative metallic dust influx.
**[Cosmic Albedoite ($\text{CaAl}2\text{Si}4\text{O}{11}$ variant)](/entries/cosmic-albedoite/($\text{CaAl}2\text{Si}4\text{O}{11}$-v…