Sanjuanite is a rare phosphate-sulfate mineral typically found as white, earthy, or chalky masses. It is most commonly identified in hydrothermal alteration zones and is frequently associated with other aluminum-bearing sulfates.
Is this sanjuanite?
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 sanjuanite with a known reference. Sanjuanite 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. Sanjuanite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Sanjuanite typically shows a dull luster.
- 4Match the color rangeCompare against the expected color range: white.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: massive, crusts, earthy.
Often confused with
Sanjuanite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside sanjuanite
Minerals reported to co-occur with sanjuanite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Al₂(PO₄)(SO₄)(OH)·9H₂O
- Mohs hardness
- 3.5
- Density
- 2.47 g/cm³
- Colors
- Streak
- White
- Luster
- Dull
- Transparency
- Opaque
- Crystal system
- Monoclinic
- Crystal habit
- Massive, Crusts, Earthy
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Alteration Zones in Volcanic Rocks
- Typical price
- $20-100 per specimen
Where rockhounds find sanjuanite
Classic worldwide localities
- San Juan, Argentina
- Cerro de los Colorados, Argentina
Field-hunting tip
Look in hydrothermal alteration zones in volcanic rocks country — that is the host setting where sanjuanite typically forms. If you start seeing alunite, jarosite, gypsum in float, you are in the right ground. Field specimens usually show a massive, crusts, earthy habit, so train your eye for that shape before scanning the outcrop.



