Demartinite is an extremely rare potassium fluorosilicate mineral found primarily as a fumarolic sublimation product at Mount Vesuvius. It typically forms small, yellow, tabular crystals or delicate crusts in volcanic vents where fluorine-rich gases have interacted with the local environment.
Is this demartinite?
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 demartinite with a known reference. Demartinite sits at Mohs 2, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Demartinite leaves a yellowish streak.
- 3Read the lusterHold the specimen under a strong light. Demartinite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, yellowish-green.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: tabular crystals, crusts.
Often confused with
Demartinite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside demartinite
Minerals reported to co-occur with demartinite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- K₂SiF₆
- Mohs hardness
- 2
- Density
- 2.65 g/cm³
- Colors
- Streak
- Yellowish
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Tabular Crystals, Crusts
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Fumarolic Deposits
- Typical price
- $50-300 per specimen
Where rockhounds find demartinite
Classic worldwide localities
- Vesuvius (Italy)
Field-hunting tip
Look in fumarolic deposits country, the host setting where demartinite typically forms. If you start seeing malladrite, avogadrite, salmiac in float, you are in the right ground. Field specimens usually show a tabular crystals, crusts habit, so train your eye for that shape before scanning the outcrop.



