Diaoyudaoite is a rare sodium aluminate mineral discovered in heavy mineral sands. It typically occurs as small, colorless tabular crystals and is noted for its unique composition relative to more common aluminum-bearing minerals.
Is this diaoyudaoite?
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 diaoyudaoite with a known reference. Diaoyudaoite sits at Mohs 7.6, 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: vitreous.
- 4Match the color rangeCompare against the expected color range: colorless, light green.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: tabular crystals.
Often confused with
Diaoyudaoite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside diaoyudaoite
Minerals reported to co-occur with diaoyudaoite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- NaAl₁₁O₁₇
- Mohs hardness
- 7.6
- Density
- 3.30 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Hexagonal
- Crystal habit
- Tabular crystals
- Cleavage
- One direction, good
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In the heavy-mineral (S.G. > 2.8) fraction of the surface layer of sea-floor muds at about 1500 m water depth
Where rockhounds find diaoyudaoite
Classic worldwide localities
- Okinawa Trough, near Diaoyudao Island, a few km northeast of Taiwan
Field-hunting tip
Where it forms: In the heavy-mineral (S.G. > 2.8) fraction of the surface layer of sea-floor muds at about 1500 m water depth. If you start seeing chromium inclusions, epidote, dolomite in float, you are in the right ground. Typical habit: tabular crystals. Train your eye for that shape before scanning the outcrop.







