Iron Monoxide: Difference between revisions

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Iron monoxide consists of divalent iron (Fe²⁺) bound to oxygen, forming a basic oxide.

It oxidizes further to Fe₂O₃ or Fe₃O₄ upon exposure to air.

In plasma environments such as [[Ignispheric]] worlds, vaporized FeO emits green light and conducts psionic current—forming “iron rain.”

In plasma environments such as [[Ignispheric Atmosphere]] worlds, vaporized FeO emits green light and conducts psionic current—forming “iron rain.”

== Phases ==

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* Indicator of reducing atmospheres and molten metal cycles.

* Ingredient in divine forges, symbolizing balance between order (metal) and decay (oxide).

* Observed in the atmospheres of volcanic [[Permian-like Atmosphere]] and [[Ignispheric]] worlds.

* Observed in the atmospheres of volcanic [[Permian-like Atmosphere]] and [[Ignispheric Atmosphere]] worlds.

== Related Atmospheres ==

* [[Ignispheric]]

* [[Ignispheric Atmosphere]]

* [[Permian-like Atmosphere]]

== Trivia ==

* The term “iron rain” originates from divine chronicles describing molten droplets condensing in the upper forges of [[Ignispheric]] planets.

* The term “iron rain” originates from divine chronicles describing molten droplets condensing in the upper forges of [[Ignispheric Atmosphere]] planets.

* FeO crystals retain weak psionic magnetism, used in constructing memory compasses.