Clinobisvanite is a rare bismuth vanadate mineral that typically forms as small, tabular yellow-to-orange crystals in oxidized bismuth ore deposits. It is best identified by its high density, adamantine luster, and association with other bismuth secondary minerals. Due to its scarcity and fragility, it is highly sought after by specialized systematic mineral collectors.
Is this clinobisvanite?
5-step field checkRun through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.
- 1Test the hardnessTry to scratch clinobisvanite with a known reference. Clinobisvanite sits at Mohs 3-4 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Clinobisvanite leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Clinobisvanite typically shows a adamantine luster.
- 4Match the color rangeCompare against the expected color range: yellow, orange-yellow, reddish-brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals, platy, crusts.
Often confused with
Clinobisvanite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside clinobisvanite
Minerals reported to co-occur with clinobisvanite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- BiVO₄
- Mohs hardness
- 3-4
- Density
- 6.9-7.0 g/cm³
- Streak
- Yellow
- Luster
- Adamantine
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular Crystals, Platy, Crusts
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Bismuth-bearing Hydrothermal Veins
- Typical price
- $50-500 depending on specimen size and quality
Where rockhounds find clinobisvanite
Classic worldwide localities
- Schneeberg, Germany
- Goldfield, Nevada, USA
- Miaogou, China
- Tsumeb, Namibia
Field-hunting tip
Look in oxidized bismuth-bearing hydrothermal veins country — that is the host setting where clinobisvanite typically forms. If you start seeing bismutite, bismutheite, quartz in float, you are in the right ground. Field specimens usually show a tabular crystals, platy, crusts habit, so train your eye for that shape before scanning the outcrop.





