kaldrlmasyla

Kaldrlmasyla is a rare crystalline mineral noted for its capacity to store thaumic energy and for a dim, moonlit glow. It forms in high-temperature hydrothermal veins and is most commonly found in basaltic regions of the southern arcipelago of Nyr. The mineral typically appears as small, tabular crystals intergrown with magnetite and amphibole. Its color ranges from clear to pale blue, and under low-tech lighting it exhibits a soft luminescence that intensifies near thaumic fields.

The term kaldrlmasyla derives from the old kaldri and masyla dialects, where it is interpreted as “light-bound stone.” It was first described in the expedition records of the Lathari Survey in the early medieval period, and the name has since become standard in mineralogical and magical treatises.

Kaldrlmasyla has a non-stoichiometric, silicate-rich framework with trace rare-earth elements. Its precise chemical composition varies between deposits, but it consistently demonstrates high dielectric properties and energy storage capacity. The mineral responds to ritual energy flows by altering its lattice vibrations, enabling rapid release or absorption of thaumic pulses.

Deposits are typically small and dispersed, requiring careful, low-impact extraction methods to minimize dendritic fracturing of host rocks. Large-scale mining is limited by the mineral’s rarity and fragmented distribution.

In practical use, kaldrlmasyla is employed to stabilize energy conduits, inscribe runes, and power compact sigils. Economically, it commands high value but remains sensitive to ethical and ecological considerations.