Flinteite is a rare potassium fluorosilicate typically found as a secondary mineral in volcanic fumaroles. It most commonly occurs as small, delicate tabular crystals often associated with other fluorine-bearing minerals.
Is this flinteite?
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 flinteite with a known reference. Flinteite 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. Flinteite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Flinteite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: white, yellow, brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals.
Often confused with
Flinteite vs. its common look-alikes — and how to tell them apart in the field.

How to tell apart: Flinteite is noticeably harder (Mohs 3.5 vs. 2); luster reads pearly on Flinteite and vitreous on Malladrite.

How to tell apart: Flinteite is noticeably harder (Mohs 3.5 vs. 2); luster reads pearly on Flinteite and vitreous on Hieratite.
Often found alongside flinteite
Minerals reported to co-occur with flinteite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- K₂SiF₆
- Mohs hardness
- 3.5
- Density
- 2.5 g/cm³
- Streak
- White
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular Crystals
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Fumarolic Deposits
- Typical price
- $50-200 per specimen
Where rockhounds find flinteite
Classic worldwide localities
- Fumaroles at La Fossa crater, Vulcano, Italy
Field-hunting tip
Look in fumarolic deposits country — that is the host setting where flinteite typically forms. If you start seeing malladrite, hieratite, sulfur in float, you are in the right ground. Field specimens usually show a tabular crystals habit, so train your eye for that shape before scanning the outcrop.

