Changbaiite is an extremely rare lead niobate mineral found in specific alkaline pegmatites. It typically occurs as small, colorless tabular crystals and is prized primarily by mineralogists and advanced systematic collectors.
Is this changbaiite?
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 changbaiite with a known reference. Changbaiite sits at Mohs 5.3, 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: adamantine to pearly.
- 4Match the color rangeCompare against the expected color range: colorless, cream white, pale brown, yellow brown, pale yellow green.
- 5Look at form & habitCrystal system: trigonal. Typical habit: tabular.
Often confused with
Changbaiite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside changbaiite
Minerals reported to co-occur with changbaiite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- PbNb₂O₆
- Mohs hardness
- 5.3
- Density
- 6.48 g/cm³
- Colors
- Streak
- White
- Luster
- Adamantine to pearly
- Transparency
- Transparent to translucent
- Crystal system
- Trigonal
- Crystal habit
- Tabular
- Cleavage
- {0001}, perfect; one rhombohedral, distinct
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In kaolinite-filled veins and cavities in a potassic granite
Where rockhounds find changbaiite
Classic worldwide localities
- Changbai Mountain, Tonghua, southeastern Kirin Province, China
Field-hunting tip
Where it forms: In kaolinite-filled veins and cavities in a potassic granite. If you start seeing kaolinite, quartz, potassic feldspar in float, you are in the right ground. Typical habit: tabular. Train your eye for that shape before scanning the outcrop.



