Romanorlovite is an exceptionally rare mercury-potassium chloride mineral found primarily in volcanic fumaroles. It typically occurs as small, sharp octahedral crystals with a distinct yellow color and high luster, often forming in low-temperature volcanic vent environments.
Is this romanorlovite?
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 romanorlovite with a known reference. Romanorlovite sits at Mohs ~3, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: yellow.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: yellow-brown, dark brown.
- 5Look at form & habitCrystal system: tetragonal.
Often confused with
Romanorlovite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside romanorlovite
Minerals reported to co-occur with romanorlovite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- K₁₁Cu₉Cl₂₅(OH)₄·2H₂O
- Mohs hardness
- ~3
- Density
- 2.61 g/cm³
- Colors
- Streak
- Yellow
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Tetragonal
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- As sublimates around active fumaroles
Where rockhounds find romanorlovite
Classic worldwide localities
- Glavnaya Tenoritovaya and Arsenatnaya fumaroles, Second scoria cone, Northern Breakthrough of the Great Tolbachik Fissure Eruption, Tolbachik volcano, Kamchatka, Russia
Field-hunting tip
Where it forms: As sublimates around active fumaroles. If you start seeing hematite, pseudobrookite, clinoenstatite in float, you are in the right ground.






