Markhininite is an extremely rare silver telluride mineral first described from the Kochbulak deposit in Uzbekistan. It typically occurs as microscopic grains associated with other telluride species in hydrothermal gold-bearing veins, making it primarily of interest to advanced mineral collectors and researchers.
Is this markhininite?
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 markhininite with a known reference. Markhininite sits at Mohs 1.5-2 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Markhininite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Markhininite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: white, colorless, grayish.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: granular, massive, as small inclusions.
Often confused with
Markhininite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside markhininite
Minerals reported to co-occur with markhininite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ag₂Te
- Mohs hardness
- 1.5-2
- Density
- 8.8-9.0 g/cm³
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Monoclinic
- Crystal habit
- Granular, Massive, As Small Inclusions
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Epithermal Gold-telluride Deposits
- Typical price
- $50-500+ for micro-specimens
Where rockhounds find markhininite
Classic worldwide localities
- Kochbulak deposit, Uzbekistan
Field-hunting tip
Look in epithermal gold-telluride deposits country — that is the host setting where markhininite typically forms. If you start seeing gold, hessite, coloradoite in float, you are in the right ground. Field specimens usually show a granular, massive, as small inclusions habit, so train your eye for that shape before scanning the outcrop.







