Khrenovite is a rare arsenate mineral discovered in the volcanic fumaroles of the Tolbachik volcano in Russia. It typically occurs as small, yellow, transparent tabular crystals associated with other volcanic sublimates.
Is this khrenovite?
4-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 khrenovite with a known reference. Khrenovite sits at Mohs 4-5, softer than the next harder reference, harder than the previous one.
- 2Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 3Match the color rangeCompare against the expected color range: yellow, yellowish-brown.
- 4Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals.
Often confused with
Khrenovite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside khrenovite
Minerals reported to co-occur with khrenovite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₃Fe³⁺₂(AsO₄)₃
- Mohs hardness
- 4-5
- Colors
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular crystals
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A sublimate at an active volcanic fumarole
Where rockhounds find khrenovite
Classic worldwide localities
- Arsenatnaya fumarole, Second scoria cone of the Northern Breakthrough of the Great Tolbachik Fissure Eruption, Tolbachik volcano, Kamchatka peninsula, Far-Eastern Region, Russia
Field-hunting tip
Where it forms: A sublimate at an active volcanic fumarole. If you start seeing hematite, tenorite, sylvite in float, you are in the right ground. Typical habit: tabular crystals. Train your eye for that shape before scanning the outcrop.





