Benleonardite is a rare silver sulfotelluride typically found as thin, dark blue-to-black coatings on other minerals in hydrothermal deposits. It is best identified through laboratory analysis of its metallic, opaque character and specific paragenesis in rare tellurium-rich ore bodies.
Is this benleonardite?
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 benleonardite with a known reference. Benleonardite sits at Mohs 1.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Benleonardite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Benleonardite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: dark blue, black, blue-black.
- 5Look at form & habitCrystal system: cubic. Typical habit: microcrystalline aggregates, crusts.
Often confused with
Benleonardite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside benleonardite
Minerals reported to co-occur with benleonardite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ag₈(Sb,As)Te₂S₃
- Mohs hardness
- 1.5
- Density
- 8.09 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Microcrystalline Aggregates, Crusts
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Tellurium-bearing Hydrothermal Veins
- Typical price
- $100-500 per specimen
Where rockhounds find benleonardite
Classic worldwide localities
- Bambolla mine, Mexico
- Moctezuma, Mexico
Field-hunting tip
Look in tellurium-bearing hydrothermal veins country — that is the host setting where benleonardite typically forms. If you start seeing bambollaite, diaoyudaoite, tellurium in float, you are in the right ground. Field specimens usually show a microcrystalline aggregates, crusts habit, so train your eye for that shape before scanning the outcrop.




