Chaidamuite is a rare secondary sulfate mineral typically found as small, yellow, translucent crystals in the oxidation zones of ore deposits. It is named after its type locality in the Qaidam Basin of China and is highly sought after by collectors of rare sulfate species.
Is this chaidamuite?
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 chaidamuite with a known reference. Chaidamuite sits at Mohs 2.5-3, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: pale yellow.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: brown, yellowish brown.
- 5Look at form & habitCrystal system: triclinic. Typical habit: prismatic, tabular.
Often confused with
Chaidamuite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside chaidamuite
Minerals reported to co-occur with chaidamuite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- ZnFe³⁺(SO₄)₂(OH)·4H₂O
- Mohs hardness
- 2.5-3
- Density
- 2.722 g/cm³
- Colors
- Streak
- Pale yellow
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Triclinic
- Crystal habit
- Prismatic, tabular
- Cleavage
- On {001} and {100}, perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A secondary mineral in the oxidized portions of a Pb–Zn–Fe sulfide deposit
Where rockhounds find chaidamuite
Classic worldwide localities
- Xitieshan Pb–Zn mine, south of Mt. Qilianshan, Chaidamu, Qinghai Province, China
Field-hunting tip
Where it forms: A secondary mineral in the oxidized portions of a Pb–Zn–Fe sulfide deposit. If you start seeing coquimbite, copiapite, butlerite in float, you are in the right ground. Typical habit: prismatic, tabular. Train your eye for that shape before scanning the outcrop.




