Petersite-(La) is a rare secondary mineral typically found as fine, acicular, or fibrous radial sprays in oxidized copper deposits. It is most recognized for its vibrant blue to blue-green color and its association with other copper-bearing minerals like malachite.
Is this petersite-(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 petersite-(la) with a known reference. Petersite-(La) 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. Petersite-(La) leaves a pale blue streak.
- 3Read the lusterHold the specimen under a strong light. Petersite-(La) typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: blue, blue-green, green.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: acicular or fibrous radial clusters.
Often confused with
Petersite-(La) vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside petersite-(la)
Minerals reported to co-occur with petersite-(la). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (La,Ce,Nd,Ca)Cu₆(PO₄)₃(OH)₆·3H₂O
- Mohs hardness
- 3-4
- Density
- 4.2-4.5 g/cm³
- Colors
- Streak
- Pale Blue
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Hexagonal
- Crystal habit
- Acicular or Fibrous Radial Clusters
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Copper-bearing Hydrothermal Deposits
- Typical price
- $50-300 per specimen depending on size and quality
Where rockhounds find petersite-(la)
Classic worldwide localities
- China
- Czech Republic
- France
Field-hunting tip
Look in oxidized copper-bearing hydrothermal deposits country — that is the host setting where petersite-(la) typically forms. If you start seeing malachite, azurite, limonite in float, you are in the right ground. Field specimens usually show a acicular or fibrous radial clusters habit, so train your eye for that shape before scanning the outcrop.





