Kuznetsovite is a rare mercury-arsenic oxychloride mineral that typically forms small, distinct tetrahedral crystals. It is primarily found in the unique hydrothermal environment of the Khaidarkan mercury-antimony deposit. Due to its toxic mercury and arsenic content and extreme rarity, it is sought after primarily by advanced mineral collectors.
Is this kuznetsovite?
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 kuznetsovite with a known reference. Kuznetsovite sits at Mohs 3.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Kuznetsovite leaves a yellow-orange streak.
- 3Read the lusterHold the specimen under a strong light. Kuznetsovite typically shows a adamantine luster.
- 4Match the color rangeCompare against the expected color range: dark red, red-brown, orange-red.
- 5Look at form & habitCrystal system: cubic. Typical habit: tetrahedral crystals, massive.
Often confused with
Kuznetsovite vs. its common look-alikes — and how to tell them apart in the field.

How to tell apart: Kuznetsovite is noticeably harder (Mohs 3.5 vs. 2-2.5); streak differs — Kuznetsovite leaves yellow-orange, Cinnabar leaves scarlet.

How to tell apart: Streak differs — Kuznetsovite leaves yellow-orange, Kleinite leaves white.
Often found alongside kuznetsovite
Minerals reported to co-occur with kuznetsovite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Hg₃AsO₄Cl
- Mohs hardness
- 3.5
- Density
- 6.8 g/cm³
- Streak
- Yellow-orange
- Luster
- Adamantine
- Transparency
- Translucent
- Crystal system
- Cubic
- Crystal habit
- Tetrahedral Crystals, Massive
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Mercury-antimony Hydrothermal Deposits
- Typical price
- $100-500 thumbnail
Where rockhounds find kuznetsovite
Classic worldwide localities
- Khaidarkan antimony-mercury deposit, Kyrgyzstan
Field-hunting tip
Look in mercury-antimony hydrothermal deposits country — that is the host setting where kuznetsovite typically forms. If you start seeing cinnabar, calomel, eglestonite in float, you are in the right ground. Field specimens usually show a tetrahedral crystals, massive habit, so train your eye for that shape before scanning the outcrop.



