Feynmanoctonaspar

Feynmanoctonaspar is the crystal mineral form of Si3(OF2)CaOt•Fy3(RaN). It has a light blue glow due to its radioactivity combined from its radiation-emitting elements Radium, Octonium and Feynmanium. This element breaks down in air forming Nitric Oxide, Calcium Monofluorosilicate [CaSi(F)], Octonium Radate [OtRaO - ] (dash meaning unknown) & Feynmanium Disilicate [FySi 2 ]. The One fluorine is pushed out to form Oxygen Fluoride which is a reactive explosive. This is why when this mineral is exposed to air, it explodes and usually burns itself from the heat and radiation. In moist air, this mineral tends to glow releasing fluorine gas from it causing again, explosions...

The Most Easiest way to make it is by adding a Silicic Acid solution to a high point beaker, leaving it for a few days under a vacuum chamber leaving Silicon Dioxide.

Si(O4H4) → SiO2

One this Silicon Dioxide is made, you would need to add it to some Calcium Fluoride [CaF2]. This reacts to form Calcium Monofluorosilicate [CaSi(F)]

SiO2 + CaF2 → CaSiF2 + O → OF(Ejected) → CaSi(F)

Once this process is done, you will need Radium Nitride [Ra3N2] (which is present on radium) and add it to the Calcium Solution

CaSi(F) + Ra3N2 → RaF(SiCa)N + N