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, 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.




