Fotomultipliatorite

Fotomultipliatorite is a rare mineral discovered in 2016, found in the Kola Peninsula, Russia. It is named after its unique photomultiplication property, where it can produce multiple copies of itself when exposed to light. This property is due to its complex crystal structure, which allows it to absorb and re-emit photons, leading to the formation of new crystals.

Fotomultipliatorite is a silicate mineral, with a chemical formula of (Na,K)2Ca2(Si8O20)2. It crystallizes in the monoclinic system, with a hardness of 5.5 on the Mohs scale. Its color ranges from colorless to pale yellow, and it has a vitreous luster. The mineral is typically found in small, prismatic crystals, often associated with other silicate minerals such as nepheline and sodalite.

The discovery of fotomultipliatorite has sparked interest in the scientific community, as it represents a new class of minerals with unique properties. Further research is needed to fully understand the mechanisms behind its photomultiplication and to explore potential applications in fields such as materials science and nanotechnology.