Ilesite is a rare manganese-bearing sulfate mineral typically found as secondary crusts or coatings in oxidizing sulfide deposits. It is highly unstable in humid conditions and can easily dehydrate into other sulfate species, so it should be stored in a cool, dry, and airtight container.
Is this ilesite?
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 ilesite with a known reference. Ilesite sits at Mohs 2-3, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: green, greenish white, white.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: aggregates, encrustations.
Often confused with
Ilesite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside ilesite
Minerals reported to co-occur with ilesite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- MnSO₄·4H₂O
- Mohs hardness
- 2-3
- Density
- 2.26 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Aggregates, encrustations
- Cleavage
- Good
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A rare secondary mineral in the oxidized zones of sulfide deposits
Where rockhounds find ilesite
Classic worldwide localities
- McDonnell claim, Montezuma district, Hall Valley, Park Co., and at the Penn mine, Summit Co., Colorado, USA
- Silver King mine, Galena Hill, Yukon Territory, Canada
- Chvaletice, Czech Republic
- Jokoku mine, southwest Hokkaido, Japan
Field-hunting tip
Where it forms: A rare secondary mineral in the oxidized zones of sulfide deposits. If you start seeing pyrite, sphalerite, galena in float, you are in the right ground. Typical habit: aggregates, encrustations. Train your eye for that shape before scanning the outcrop.







