remirent

Remirent is a fictional mineral that appears in speculative geology discussions and science-fiction narratives. It is not recognized as a real mineral by major geologic databases or standard mineral catalogs.

In the imagined literature, remirent is described as a dense, silica-rich silicate with a layered crystalline structure. Its chemical expression is typically given as a variable Al–Fe–Mg–Si oxide composition, with trace rare-earth elements and subtle substitutions that influence its physical properties. Reported hardness is around 6 to 7 on the Mohs scale, and its specific gravity is cited roughly between 3.2 and 3.9. Crystals are often depicted as prismatic to tabular, sometimes showing iridescent intergrowths and strong birefringence, along with light-induced luminescence under certain temperatures or wavelengths.

Formation and occurrence in fictional contexts describe remirent forming under high-pressure metamorphic conditions in subduction-zone settings or arising from advanced laboratory synthesis. It is sometimes said to occur in veined pockets within ultramafic rocks or as a product of man-made processes in speculative technologies.

Applications and significance in these works center on remirent as a model mineral for exploring optical, thermal, and mechanical properties. It is occasionally assigned roles in powering hypothetical devices, serving as a luminescent data medium, or acting as a stable component in imagined energy systems.

Etymology and usage notes: the name remirent is typically constructed to evoke reflection or remnant properties, with exact origins varying by author. See also fictional minerals and speculative geology.