Quenstedtite is a rare hydrated iron sulfate mineral typically found as a secondary product in the oxidized zones of ore deposits. It is known for its distinct pale violet color, though it is highly soluble and must be kept away from humidity to prevent dehydration or degradation.
Is this quenstedtite?
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 quenstedtite with a known reference. Quenstedtite sits at Mohs 2.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Quenstedtite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Quenstedtite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: violet, pale lilac, yellowish.
- 5Look at form & habitCrystal system: triclinic. Typical habit: tabular crystals, crusts, granular aggregates.
Often confused with
Quenstedtite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside quenstedtite
Minerals reported to co-occur with quenstedtite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Fe₂(SO₄)₃·11H₂O
- Mohs hardness
- 2.5
- Density
- 2.04 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Triclinic
- Crystal habit
- Tabular Crystals, Crusts, Granular Aggregates
- Cleavage
- Good On {010}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Zones of Iron-rich Sulfide Deposits
- Typical price
- $50-300 per specimen depending on size and quality
Where rockhounds find quenstedtite
Classic worldwide localities
- Tierra Amarilla, Chile
- Chuquicamata, Chile
- Alcaparrosa Mine, Chile
Field-hunting tip
Look in oxidized zones of iron-rich sulfide deposits country — that is the host setting where quenstedtite typically forms. If you start seeing copiapite, coquimbite, jarosite in float, you are in the right ground. Field specimens usually show a tabular crystals, crusts, granular aggregates habit, so train your eye for that shape before scanning the outcrop.




