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, 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.

