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Leucophanite is a rare fluorescent mineral prized by collectors for its striking UV luminescence and rarity. This unique mineral, with the chemical formula (Na,Ca)₂BeSi₂(O,OH,F)₇, often contains cerium substitutions, making each specimen chemically distinctive.

Found in only a few locations globally—including Norway, Quebec, and Russia—massive habit leucophanite specimens suitable for display are known to come exclusively from Norway. These pieces are highly sought after for their aesthetic beauty and rarity on the mineral market.

Norwegian leucophanite typically appears in yellow, white, or greenish triclinic crystals, and is often associated with alkaline igneous complexes and pegmatites. The finest examples are bright and vividly fluorescent, exhibiting spectacular reactions under both midwave and shortwave UV light. Shortwave UV brings out brilliant yellow fluorescence from embedded zircon inclusions, enhancing their visual appeal for UV mineral collectors.

Discovered in the Langesundsfjord district of southern Norway in 1840, leucophanite derives its name from the Greek "leukos" (white) and "phanein" (to appear), referencing its common pale coloration.
Due to its rarity and limited geographic occurrence, high-quality leucophanite specimens are rarely available—especially in larger sizes. When they do surface, they are considered top-tier additions to any fluorescent mineral collection or museum-grade mineral display.