Kraisslite is a rare zinc manganese magnesium hydroxide, typically deep coppery brown. It occurs in a metamorphosed stratiform zinc deposit. It was first described from Sterling Hill, Ogdensburg, Sussex Co., New Jersey, USA.
Is this kraisslite?
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 kraisslite with a known reference. Kraisslite sits at Mohs 3, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Kraisslite leaves a golden brown streak.
- 3Read the lusterHold the specimen under a strong light. Kraisslite typically shows a submetallic luster.
- 4Match the color rangeCompare against the expected color range: deep coppery brown.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: platy crystals, tabular aggregates.
Often confused with
Kraisslite vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Streak differs, so Kraisslite leaves golden brown, Dixenite leaves brownish-red; luster reads submetallic on Kraisslite and metallic to resinous on Dixenite.

How to tell apart: Streak differs, so Kraisslite leaves golden brown, Allactite leaves light brown; luster reads submetallic on Kraisslite and vitreous on Allactite.
Often found alongside kraisslite
Minerals reported to co-occur with kraisslite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Zn₃(Mn,Mg)₂₅(Fe³⁺,Al)(As³⁺O₃)₂[(Si,As⁵⁺)O₄]₁₀(OH)₁₆
- Mohs hardness
- 3
- Density
- 3.876 g/cm³
- Colors
- Streak
- Golden Brown
- Luster
- Submetallic
- Transparency
- Translucent
- Crystal system
- Hexagonal
- Crystal habit
- Platy Crystals, Tabular Aggregates
- Cleavage
- Perfect in One Direction
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Metamorphosed Iron-manganese Deposits
Where rockhounds find kraisslite
Classic worldwide localities
- Sterling Hill, Ogdensburg, Sussex Co., New Jersey, USA
Field-hunting tip
Look in metamorphosed iron-manganese deposits country, the host setting where kraisslite typically forms. If you start seeing hausmannite, baryte, calcite in float, you are in the right ground. Field specimens usually show a platy crystals, tabular aggregates habit, so train your eye for that shape before scanning the outcrop.



