Iowaite is a rare layered double hydroxide mineral typically found as green to blue-green platy aggregates in serpentinized rocks. It is highly unstable when exposed to air and can dehydrate or alter rapidly, making it a challenging but rewarding find for mineral collectors.
Is this iowaite?
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 iowaite with a known reference. Iowaite sits at Mohs 1.5-2.5, 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: greasy.
- 4Match the color rangeCompare against the expected color range: bluish green, greenish white, honey yellow.
- 5Look at form & habitCrystal system: trigonal. Typical habit: platy.
Often confused with
Iowaite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside iowaite
Minerals reported to co-occur with iowaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Mg₆Fe₂(OH)₁₆Cl₂·4H₂O
- Mohs hardness
- 1.5-2.5
- Density
- 2.09 g/cm³
- Streak
- White
- Luster
- Greasy
- Transparency
- Opaque to translucent
- Crystal system
- Trigonal
- Crystal habit
- Platy
- Cleavage
- {0001}, perfect
- Rarity
- Rare
- Uses
- Collector, Scientific research
- Host rock
- An alteration product of serpentine
Where rockhounds find iowaite
Classic worldwide localities
- Drill core from the Precambrian basement of Sioux Co., Iowa, USA
- Phalaborwa mine, Transvaal, South Africa
- Komsomolsk mine, Talnakh, Noril’sk region, western Siberia, Russia
- Almalyk district, Uzbekistan
- Sea floor sediments in the Bonin-Mariana area, Pacific Ocean
- Mount Keith nickel deposit, 400 km north-northwest of Kalgoorlie, Western Australia
Field-hunting tip
Where it forms: An alteration product of serpentine. If you start seeing chrysotile, dolomite, brucite in float, you are in the right ground. Typical habit: platy. Train your eye for that shape before scanning the outcrop.








