Stibivanite

Chemical formula: Sb<sup>3+</sup><sub>2</sub>V<sup>4+</sup>O<sub>5</sub>

Stibivanite is a rare antimony and vanadium oxide, characterized by a adamantine luster and occurring as small, acicular crystals.

## Characteristics Stibivanite is an antimony and vanadium oxide, typically forming small but striking aggregates. It most often occurs as aggregates of fine, acicular or prismatic crystals, which can arrange themselves into divergent, radial fans or compact, subparallel bundles. Its most characteristic visual feature is a very strong, adamantine luster, which distinguishes it from the host rock. ## Physical Properties This mineral is relatively soft, with a Mohs hardness of 4-4.5, meaning it can be scratched by a steel blade. It is translucent and exhibits a strong, adamantine luster. Its fracture is splintery, which is typical for minerals with a fibrous or acicular habit. ## Colors and Varieties Stibivanite ranges in color from yellowish-brown, through reddish-brown, to brown. No specific color or commercial varieties are known. ## History and Name The mineral was first described in 1983 by J. L. Jambor, A. C. Roberts, and A. J. Criddle. Its name directly refers to its chemical composition: it comes from the Latin word *stibium* (antimony) and the name of the element *vanadium*. The type locality (place of first discovery) was identified as Taylor Pit in the Potash Sulphur Springs area of Arkansas, USA. ## Uses Due to its rarity, stibivanite has no industrial applications. It is solely an object of interest for collectors of rare minerals and scientists.

Properties

Mohs hardness
4-4.5
Color
Yellow-green.
Luster
Adamantine
Streak
white
Density
0
Cleavage
Prismatic {210}; also weak to poor {110}.
Fracture
Splintery
Transparency
Translucent
Crystal system
Orthorhombic

Diagnostic features

## Identification Key diagnostic features of stibivanite are its characteristic, very strong adamantine luster, brown color, and acicular or prismatic crystal form creating radial aggregates. Its occurrence environment – oxidation zones of antimony deposits – is also an important indicator. ## Distinguishing from Similar Minerals Stibivanite is sometimes confused with other brown minerals with a strong luster. It is distinguished from rutile by its significantly lower hardness (rutile has a hardness of 6-6.5). It differs from some varieties of sphalerite by its crystal form (sphalerite forms isometric crystals) and lack of perfect cleavage. Its specific association with antimony minerals is also an important clue. ## Crystal Forms It crystallizes in the orthorhombic system. It forms acicular or slender prismatic crystals, elongated along one axis. These crystals almost always occur as aggregates – divergent, radial, or subparallel bundles.

Geological environment

## Genesis Stibivanite is a secondary mineral. It forms in oxidation (weathering) zones of hydrothermal deposits, as a result of the alteration of native antimony in the presence of vanadium-containing solutions. It forms in vugs and fractures within quartz veins. ## Mineral Associations It most often co-occurs with minerals from which it forms or which it accompanies. These are primarily: native antimony, stibiconite, valentinite, cervantite, and quartz. ## Localities It is a very rare mineral, known from a few localities worldwide. The most important of these is the type locality in Arkansas, USA. In addition, its occurrence has been confirmed, among others, in the Baccu Locci mine in Sardinia (Italy) and in several locations in Japan.

Rarity

Extremely Rare

For collectors

## Quality Criteria The quality of stibivanite specimens is primarily assessed based on the richness and aesthetics of the crystal aggregates. The most valued samples are those with well-formed, sharp crystals forming visually attractive, radial clusters. Intense, adamantine luster and contrast with associated minerals on the rock matrix are also highly rated. Due to the small size of the crystals, most specimens on the market are so-called micromounts (specimens for viewing under magnification). ## Popular Localities The most classic and highly valued specimens by collectors come from its first discovery site – Taylor Pit in Arkansas, USA. These serve as reference material for this species.

Care and storage

## Cleaning Stibivanite specimens should be cleaned very carefully, using a soft brush and distilled water. Due to its low hardness, strong rubbing should be avoided. Ultrasonic cleaners are not recommended, as they can damage delicate crystal aggregates. ## What to Avoid Avoid contact with strong chemicals and acids. The mineral is brittle and susceptible to mechanical damage, so it must be protected from impacts and scratching by harder minerals. There is no detailed data on its sensitivity to light or temperature, but standard caution is advised. ## Storage Collector specimens of stibivanite, especially those in the form of micromounts, are best stored in separate, sealed boxes (such as "membrane boxes" or classic micromineral boxes) to protect them from dust, moisture, and mechanical damage.

Sources

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