Ashburtonite is a rare lead-titanium silicate mineral found primarily in Western Australia. It typically occurs as tiny, thin, colorless to pale blue bladed crystals associated with other lead minerals like cerussite and plumbophyllite.
Is this ashburtonite?
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 ashburtonite with a known reference. Ashburtonite sits at Mohs 3-4 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Ashburtonite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Ashburtonite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white, pale blue.
- 5Look at form & habitCrystal system: tetragonal. Typical habit: bladed crystals.
Often confused with
Ashburtonite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside ashburtonite
Minerals reported to co-occur with ashburtonite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pb₄(Cu,◻)₂(OH)₂TiSi₄O₁₄(HCO₃)
- Mohs hardness
- 3-4
- Density
- 3.5 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Tetragonal
- Crystal habit
- Bladed Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Veins in Sedimentary Rock
- Typical price
- $100-500 thumbnail
Where rockhounds find ashburtonite
Classic worldwide localities
- Ashburton Downs, Western Australia
Field-hunting tip
Look in hydrothermal veins in sedimentary rock country — that is the host setting where ashburtonite typically forms. If you start seeing plumbophyllite, cerussite, quartz in float, you are in the right ground. Field specimens usually show a bladed crystals habit, so train your eye for that shape before scanning the outcrop.



