Velikite is a rare mercury-bearing sulfide mineral within the stannite group, often appearing as fine-grained masses. It is primarily found in association with low-temperature hydrothermal deposits, particularly those rich in mercury and antimony. Due to its scarcity and metallic appearance, it is a highly sought-after species for advanced mineral collectors.
Is this velikite?
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 velikite with a known reference. Velikite 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. Velikite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Velikite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: gray, brownish-gray.
- 5Look at form & habitCrystal system: tetragonal. Typical habit: anhedral grains, massive.
Often confused with
Velikite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside velikite
Minerals reported to co-occur with velikite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Cu₂HgSnS₄
- Mohs hardness
- 3.5
- Density
- 4.56 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Tetragonal
- Crystal habit
- Anhedral Grains, Massive
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Mercury-antimony Deposits
- Typical price
- $50-300 per specimen depending on size and quality
Where rockhounds find velikite
Classic worldwide localities
- Khaidarkan deposit, Kyrgyzstan
- Yindongpo, China
Field-hunting tip
Look in hydrothermal mercury-antimony deposits country — that is the host setting where velikite typically forms. If you start seeing cinnabar, stibnite, pyrite in float, you are in the right ground. Field specimens usually show a anhedral grains, massive habit, so train your eye for that shape before scanning the outcrop.






