Fuenzalidaite is an extremely rare sulfate mineral known from arid, evaporitic environments. It typically forms thin, glassy tabular crystals that are difficult to distinguish from associated secondary sulfates without chemical analysis.
Is this fuenzalidaite?
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 fuenzalidaite with a known reference. Fuenzalidaite 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. Fuenzalidaite leaves a yellowish streak.
- 3Read the lusterHold the specimen under a strong light. Fuenzalidaite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, brown.
- 5Look at form & habitCrystal system: trigonal. Typical habit: tabular hexagonal crystals.
Often confused with
Fuenzalidaite vs. its common look-alikes — and how to tell them apart in the field.

How to tell apart: Streak differs — Fuenzalidaite leaves yellowish, Jarosite leaves yellow.

How to tell apart: Fuenzalidaite is noticeably harder (Mohs 3.5 vs. 2.5); streak differs — Fuenzalidaite leaves yellowish, Coquimbite leaves white.
Often found alongside fuenzalidaite
Minerals reported to co-occur with fuenzalidaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- K₆(Sb,As)₄(SO₄)₄O₂
- Mohs hardness
- 3.5
- Density
- 4.55 g/cm³
- Streak
- Yellowish
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Trigonal
- Crystal habit
- Tabular Hexagonal Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Evaporite Deposits
- Typical price
- n/a (extremely rare specimen)
Where rockhounds find fuenzalidaite
Classic worldwide localities
- Minas del Sol, Chile
Field-hunting tip
Look in evaporite deposits country — that is the host setting where fuenzalidaite typically forms. If you start seeing jarosite, gypsum, halite in float, you are in the right ground. Field specimens usually show a tabular hexagonal crystals habit, so train your eye for that shape before scanning the outcrop.


