Zimbabweite is a very rare oxide mineral typically found in complex granite pegmatites. It forms small, lustrous tabular crystals with a distinct adamantine luster, making it a sought-after prize for micro-mineral collectors.
Is this zimbabweite?
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 zimbabweite with a known reference. Zimbabweite sits at Mohs 5-5.5, 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: adamantine.
- 4Match the color rangeCompare against the expected color range: yellow brown, honey yellow.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: euhedral crystals, tabular.
Often confused with
Zimbabweite vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Zimbabweite is noticeably harder (Mohs 5-5.5 vs. 3.5-4); luster reads adamantine on Zimbabweite and resinous to subadamantine on Mimetite.

How to tell apart: Zimbabweite is noticeably harder (Mohs 5-5.5 vs. 2.75-3); luster reads adamantine on Zimbabweite and resinous, subadamantine to adamantine on Wulfenite.
Often found alongside zimbabweite
Minerals reported to co-occur with zimbabweite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na(Pb,Na,K)₂(Ta,Nb,Ti)₄As₄O₁₈
- Mohs hardness
- 5-5.5
- Density
- 6.20 g/cm³
- Colors
- Streak
- White
- Luster
- Adamantine
- Transparency
- Translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Euhedral crystals, tabular
- Cleavage
- {010}, perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In a hydrothermally altered kaolinized zone of a complex rare-metal and fluorine-rich granite pegmatite
Where rockhounds find zimbabweite
Classic worldwide localities
- St. Ann’s mine, southeast of Miami, Karoi district, Zimbabwe
Field-hunting tip
Where it forms: In a hydrothermally altered kaolinized zone of a complex rare-metal and fluorine-rich granite pegmatite. If you start seeing kaolinite in float, you are in the right ground. Typical habit: euhedral crystals, tabular. Train your eye for that shape before scanning the outcrop.

