Pertlikite is a very rare member of the garnet group specifically occurring as a secondary mineral in volcanic cavities. Collectors typically find it as small, yellowish-dark olive-green to black dodecahedral crystals associated with quartz and calcite within basaltic host rocks.
Is this pertlikite?
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 pertlikite with a known reference. Pertlikite sits at Mohs 7-7.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: grayish green.
- 3Match the color rangeCompare against the expected color range: dark olive green, black.
- 4Look at form & habitCrystal system: tetragonal. Typical habit: granular.
Often confused with
Pertlikite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside pertlikite
Minerals reported to co-occur with pertlikite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- K₂(Fe²⁺,Mg)₂(Mg,Fe³⁺)₄Fe³⁺₂Al(SO₄)₁₂·18H₂O
- Mohs hardness
- 7-7.5
- Density
- 2.59 g/cm³
- Colors
- Streak
- Grayish green
- Transparency
- Translucent
- Crystal system
- Tetragonal
- Crystal habit
- Granular
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In a pyrite-bearing trachytic eruptive rock, and probably formed after the oxidation of pyrite
Where rockhounds find pertlikite
Classic worldwide localities
- Madeni Zakh, Iran
Field-hunting tip
Where it forms: In a pyrite-bearing trachytic eruptive rock, and probably formed after the oxidation of pyrite. If you start seeing metavoltine, botryogen, pyrite in float, you are in the right ground. Typical habit: granular. Train your eye for that shape before scanning the outcrop.





