Ferrohexahydrite is a rare secondary sulfate mineral that typically forms as a dehydration product of melanterite in oxidized iron-rich environments. Collectors will primarily find it as pale green to white efflorescent crusts or powdery aggregates, often requiring careful storage as it is highly unstable in humid conditions.
Is this ferrohexahydrite?
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 ferrohexahydrite with a known reference. Ferrohexahydrite 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. Ferrohexahydrite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Ferrohexahydrite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: pale green, white.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: massive, granular, or crusts.
Often confused with
Ferrohexahydrite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside ferrohexahydrite
Minerals reported to co-occur with ferrohexahydrite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- FeSO₄·6H₂O
- Mohs hardness
- 2.5
- Density
- 1.97 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Massive, Granular, Or Crusts
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Zones of Sulfide Ore Deposits
- Typical price
- $20-100 thumbnail
Where rockhounds find ferrohexahydrite
Classic worldwide localities
- Germany
- Czech Republic
- USA
- Italy
Field-hunting tip
Look in oxidized zones of sulfide ore deposits country — that is the host setting where ferrohexahydrite typically forms. If you start seeing melanterite, pyrite, copiapite in float, you are in the right ground. Field specimens usually show a massive, granular, or crusts habit, so train your eye for that shape before scanning the outcrop.






