Stichtite is a soft, vibrant lilac to purple mineral typically found in serpentinite rocks as a secondary alteration product of chromite. It is prized by lapidary enthusiasts for its ability to take a polish and is frequently associated with green serpentine in the attractive rock known as Stichtite-in-Serpentine.
Is this stichtite?
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 stichtite with a known reference. Stichtite sits at Mohs 1.5-2, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Stichtite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Stichtite typically shows a waxy luster.
- 4Match the color rangeCompare against the expected color range: lilac, purple, pink, violet.
- 5Look at form & habitCrystal system: trigonal. Typical habit: massive, micaceous, foliated aggregates.
Often confused with
Stichtite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside stichtite
Minerals reported to co-occur with stichtite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Mg₆Cr₂(OH)₁₆CO₃·4H₂O
- Mohs hardness
- 1.5-2
- Density
- 2.1-2.2 g/cm³
- Streak
- White
- Luster
- Waxy
- Transparency
- Translucent
- Crystal system
- Trigonal
- Crystal habit
- Massive, Micaceous, Foliated Aggregates
- Cleavage
- Perfect Basal
- Rarity
- Rare
- Uses
- Collector, Lapidary, Decorative
- Host rock
- Serpentinite Bodies
- Typical price
- $10-50 per specimen depending on quality and size
Where rockhounds find stichtite
Classic worldwide localities
- Dundas, Tasmania
- Barberton, South Africa
- Quebec, Canada
- Kettle River, Washington
Field-hunting tip
Look in serpentinite bodies country, the host setting where stichtite typically forms. If you start seeing serpentine, chromite, magnetite in float, you are in the right ground. Field specimens usually show a massive, micaceous, foliated aggregates habit, so train your eye for that shape before scanning the outcrop.





