Suoremmin

Suoremmin is a fictional mineral species introduced for educational illustration in geology and mineralogy. It is described as a solid silicate mineral with monoclinic crystal symmetry and a typically prismatic habit.

Etymology and discovery: The name honors the imagined Suorem region in the southern highlands; the suffix -min is common in mineral nomenclature. It first appeared in an illustrative mineral handbook and is not based on any reported real specimen.

Properties: In the fictional account, suoremmin crystallizes in the monoclinic system and exhibits a pale green to olive color, a vitreous luster, and a Mohs hardness of 5.5–6. Its tested densities range from 3.2 to 3.5 g/cm3. Cleavage is observed along one good plane, with conchoidal fracture on other surfaces. The streak is pale gray.

Occurrence and formation: Suoremmin is described as forming in medium-temperature, medium-pressure metamorphic environments, such as schistose rocks in the Suorem Highlands. It is said to occur as isolated crystals and occasional aggregates, often in association with quartz, muscovite, chlorite, and apatite.

Uses and significance: In the fictional framework, suoremmin serves as a marker mineral for metamorphic grade and timing, and is used in teaching mineral identification and crystallography. No economic value is established outside the fictional context.

Note: This article is a fictional entry for demonstration purposes; no real-world specimens have been verified.