Tanzanite is the vivid blue‑to‑violet gem variety of zoisite, famed for its saturated color and mesmerizing pleochroism. In hand, crystals flash different hues when rotated—typically blue, violet, and a warmer bronze/green axis in unheated stones. The best pieces show a rich royal blue with a hint of violet, often intensified by heat treatment that removes brownish tones.
Crystals are orthorhombic and usually prismatic, commonly flattened on one axis, with bright glassy luster and parallel striations. Most specimens originate from a single district at Merelani, Tanzania, where tanzanite occurs in graphite-rich, metamorphosed schists alongside diopside, calcite, and occasional garnet (tsavorite). Collectors prize isolated, gemmy crystals and the exceedingly rare matrix pieces perched on graphite or calcite. While small singles are accessible, fine large crystals and pristine matrix specimens are scarce and can command major prices comparable to elite classic minerals.
Discovered in 1967 near Merelani and popularized by Tiffany & Co., tanzanite rapidly became a 20th‑century gem icon. In the mineral world its reputation has steadily grown as the Merelani mines yielded superb crystals—sometimes vividly saturated and water‑clear, other times with dramatic color zoning or striking associations on graphite. The species’ appeal blends pure beauty (that unmistakable blue‑violet glow), scientific interest (strong pleochroism, heat‑sensitive color centers), and locality mystique (essentially a one‑source gem). Today, collectors at every level pursue tanzanite: beginners for affordable small crystals, and advanced collectors for unrepaired, richly colored, display‑worthy singles or rare matrix pieces—especially those with provenance from notable Merelani “blocks.”
Although zoisite occurs worldwide, true “tanzanite” of collectible quality and color is essentially unique to northern Tanzania. The localities below have produced the specimens that define the species for collectors.
The world’s tanzanite capital. Merelani (Simanjiro District; historically labeled “Arusha”) is subdivided into mining blocks that have yielded tanzanite since 1967. Crystals range from thumbnail singles to sizeable cabinet pieces, typically sharply terminated prisms with brilliant luster and strong pleochroism. Most stones are heated after recovery to develop the coveted blue‑violet—unheated pieces may show green/bronze/brown with blue‑violet axes.
Aesthetically, collectors love:
Though thousands of crystals have been mined, truly top, unrepaired, robustly colored pieces remain uncommon. Many large crystals show cleavage or internal stress, and graphite matrix can be friable—making intact, repair‑free matrix pieces exceptional.
By focusing on saturated, lively color, pristine terminations, and (when possible) rare, stable matrix associations, collectors can build a compelling suite of this modern classic—one whose beauty and singular origin make it an essential in any contemporary mineral collection.