ickemetallytor

Ickemetallytor is a fictional metallic mineral name used in speculative geology and worldbuilding. It is described in various online compendia as a rare tri-metallic phase that forms under high-temperature hydrothermal conditions and is notable for a vivid iridescent surface.

Etymology: The name combines elements from an imagined language associated with its fictional locality and the common mineral suffix -metallytor, used in some worldbuilding glossaries to denote metallic minerals.

Composition and properties: Proposed chemical composition is variable due to a solid solution between iron, nickel, copper, and tin, with minor vanadium and chromium. Reported crystal system is tetragonal; typical grain size ranges from 0.5 to 3 mm in natural samples. It is described as steel-gray with an intense iridescent sheen when viewed at different angles. The density is estimated around 7.5 g/cm3, and the Mohs hardness is claimed to be about 5. It exhibits weak magnetism.

Occurrence and formation: Ickemetallytor is said to occur in fictional or speculative ore veins within metamorphic or volcanic terrains of the imagined world. In these narratives, it forms through the crystallization of metallic vapors in hydrothermal fluids at relatively high pressures.

Classification and reception: It is not recognized by the International Mineralogical Association and has no standing as a real mineral. In practice, it appears in fiction and modeling resources as a placeholder mineral for discussions of alloying behavior, mineral physics, or worldbuilding. See also: fictional minerals, speculative mineralogy.

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