Paratooite-(La) is a rare copper-lanthanum carbonate mineral typically found as small, yellow, platy crystals or thin crusts. It is primarily known from the oxidized zones of copper deposits in South Australia, often associated with other secondary copper carbonates.
Is this paratooite-(la)?
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 paratooite-(la) with a known reference. Paratooite-(La) sits at Mohs 4, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: pale blue.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous to pearly.
- 4Match the color rangeCompare against the expected color range: pale blue.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: aggregates, radial, wheat sheaf.
Often confused with
Paratooite-(La) vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside paratooite-(la)
Minerals reported to co-occur with paratooite-(la). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (La,Ca,Na,Sr)₆Cu(CO₃)₈
- Mohs hardness
- 4
- Density
- 3.68 g/cm³
- Colors
- Streak
- Pale blue
- Luster
- Vitreous to pearly
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Aggregates, radial, wheat sheaf
- Cleavage
- None observed, TEM suggests cleavage on {100}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A secondary weathering mineral in a mineralized dolomitic slatestone cut by chalcopyrite and magnetite-bearing quartz veins
Where rockhounds find paratooite-(la)
Classic worldwide localities
- Paratoo Copper Mine, 30 km southwest of Yunta, on the western edge of the Olary Province, South Australia
Field-hunting tip
Where it forms: A secondary weathering mineral in a mineralized dolomitic slatestone cut by chalcopyrite and magnetite-bearing quartz veins. If you start seeing kamphaugite-, donnayite-, bastnssite- in float, you are in the right ground. Typical habit: aggregates, radial, wheat sheaf. Train your eye for that shape before scanning the outcrop.




