Kolymite is a rare copper-mercury amalgam found in gold-bearing hydrothermal veins. It typically presents as metallic, silvery-white massive or granular aggregates and is highly sought after by advanced mineral collectors due to its unique chemical composition and limited locality availability.
Is this kolymite?
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 kolymite with a known reference. Kolymite 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. Kolymite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Kolymite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: silvery white, gray.
- 5Look at form & habitCrystal system: cubic. Typical habit: massive, anhedral grains.
Often confused with
Kolymite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside kolymite
Minerals reported to co-occur with kolymite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Cu₇Hg₆
- Mohs hardness
- 3.5
- Density
- 12.8-13.0 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Massive, Anhedral Grains
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Gold Deposits
- Typical price
- $50-300 per specimen depending on size
Where rockhounds find kolymite
Classic worldwide localities
- Kolyma River basin, Magadan Oblast, Russia
Field-hunting tip
Look in hydrothermal gold deposits country, the host setting where kolymite typically forms. If you start seeing gold, quartz, stibnite in float, you are in the right ground. Field specimens usually show a massive, anhedral grains habit, so train your eye for that shape before scanning the outcrop.




