Malladrite is a rare sodium fluorosilicate typically found as a volcanic sublimated mineral in fumaroles. It often occurs as tiny, thin hexagonal plates or white crusts associated with other fluorine-bearing minerals. Because it is water-soluble and chemically unstable in humid environments, specimens should be stored in a dry, airtight container.
Is this malladrite?
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 malladrite with a known reference. Malladrite sits at Mohs 3, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous to greasy.
- 4Match the color rangeCompare against the expected color range: rose, colorless, white.
- 5Look at form & habitCrystal system: trigonal. Typical habit: crystalline, prismatic.
Often confused with
Malladrite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside malladrite
Minerals reported to co-occur with malladrite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₂SiF₆
- Mohs hardness
- 3
- Density
- 2.755 g/cm³
- Streak
- White
- Luster
- Vitreous to greasy
- Transparency
- Semitransparent
- Crystal system
- Trigonal
- Crystal habit
- Crystalline, prismatic
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- As a volcanic sublimate
Where rockhounds find malladrite
Classic worldwide localities
- Vesuvius, Campania, and on Vulcano, Lipari Islands, Italy
Field-hunting tip
Where it forms: As a volcanic sublimate. If you start seeing avogadrite, hieratite, sal ammoniac in float, you are in the right ground. Typical habit: crystalline, prismatic. Train your eye for that shape before scanning the outcrop.







