Legrandite is a rare zinc arsenate renowned for its luminous lemon- to canary-yellow color and elegant, radiating crystal sprays. The best crystals are strikingly bright and transparent to translucent, forming fine prismatic to acicular needles with glassy luster. While it occurs at several localities, it is overwhelmingly associated with Mexico, where a few legendary finds produced the world’s finest specimens. Aesthetic contrasts against dark limonitic matrix or with associated zinc minerals (smithsonite, adamite) make legrandite a cornerstone of arsenate suites and Mexican classic collections.
Crystals range from delicate clusters only a few millimeters long to showy sprays measuring several centimeters across; exceptional Ojuela Mine groups exceed 10 cm and are among the most coveted yellow secondary minerals in the hobby. Because legrandite is scarce and fragile, truly fine, undamaged clusters are rare and command strong prices. The species is also historically important: it was first described from the Flor de Peña Mine in Nuevo León, Mexico, cementing Mexico’s preeminence for the species.
Legrandite sits high on many collectors’ wish lists for three reasons:
Availability is limited. Ojuela Mine produced several significant waves of material during the late 20th and early 21st centuries; even then, most pieces were small and/or fragile. Today, competition for top-quality, unrepaired sprays is intense. Miniatures and thumbnails with strong color and minimal damage trade briskly; cabinet-sized, pristine clusters on attractive matrix can reach top-tier prices. The species’ combination of rarity, fragility, and unmistakable aesthetics ensures enduring demand.
The Ojuela Mine (Mapimí, Durango) is unequivocally the world’s premier source of legrandite. Multiple production pulses yielded dazzling sprays and divergent bouquets of lemon-yellow prisms, commonly perched on brown to black limonitic goethite and often accompanied by adamite, smithsonite, calcite, or hemimorphite. Outstanding examples show:
Most crystals formed in oxidized cavities; many were contacted or broken in situ, so intact, unrepaired matrix clusters are scarce. Ojuela sets the standard for size, brightness, and sculptural aesthetics in legrandite, and the finest pieces rank among the most iconic secondary mineral specimens of Mexico.
The type locality for legrandite, the Flor de Peña Mine (Lampazos de Naranjo, Nuevo León), produced historically significant crystals and small clusters. Though generally smaller and less abundant than Ojuela material, Flor de Peña specimens are valued for:
Because quality pieces are limited and many ended up in early institutional or private holdings, any well-documented type-locality legrandite—especially with attractive aesthetics—commands a premium.
In general, buy from trusted sources and use a loupe and (optionally) longwave UV to probe for modern adhesives.
Legrandite is a fragile, hydrated zinc arsenate and contains arsenic—handle with care.
Following these guidelines will preserve the vivid color and delicate architecture that make legrandite one of the most admired secondary species in mineral collecting.