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 2 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Malladrite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Malladrite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white.
- 5Look at form & habitCrystal system: trigonal. Typical habit: small hexagonal plates, crusts, or encrustations.
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
- 2
- Density
- 2.8 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Trigonal
- Crystal habit
- Small Hexagonal Plates, Crusts, Or Encrustations
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Fumarolic Deposits in Volcanic Settings
- Typical price
- $50-300 per specimen
Where rockhounds find malladrite
Classic worldwide localities
- Mount Vesuvius, Italy
- Tolbachik volcano, Russia
Field-hunting tip
Look in fumarolic deposits in volcanic settings country — that is the host setting where malladrite typically forms. If you start seeing hieratite, sulfur, gypsum in float, you are in the right ground. Field specimens usually show a small hexagonal plates, crusts, or encrustations habit, so train your eye for that shape before scanning the outcrop.




