Kovovsuch
Kovovsuch is a term used to describe a rare geological phenomenon characterized by the spontaneous formation of metallic crystalline structures in subterranean environments. These structures are typically found within deep cave systems or volcanic calderas, where specific mineral compositions and extreme pressure conditions are present. The metallic elements involved in Kovovsuch formation are varied, but commonly include iron, nickel, and trace amounts of platinum or gold.
The exact process by which Kovovsuch forms is still a subject of scientific research. Current hypotheses suggest
Kovovsuch is not a naturally occurring mineral in the traditional sense but rather a macro-scale aggregation