Pseudograndreefite is an extremely rare lead sulfate fluoride mineral found primarily in the oxidation zones of hydrothermal lead deposits. Collectors should look for its characteristic adamantine luster and tabular crystal habit in specimens from the Grand Reef Mine.
Is this pseudograndreefite?
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 pseudograndreefite with a known reference. Pseudograndreefite sits at Mohs ~2.5, 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: subadamantine.
- 4Match the color rangeCompare against the expected color range: colorless.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: tabular crystals.
Often confused with
Pseudograndreefite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside pseudograndreefite
Minerals reported to co-occur with pseudograndreefite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pb₆SO₄F₁₀
- Mohs hardness
- ~2.5
- Density
- 7.0 g/cm³
- Colors
- Streak
- White
- Luster
- Subadamantine
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Tabular crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In a vug isolated from acidic sulfate-rich solutions in the oxidized zone of a low-temperature Pb–Cu–Ag deposit
Where rockhounds find pseudograndreefite
Classic worldwide localities
- Grand Reef mine, about six km northeast of Klondyke, Aravaipa district, Graham Co., Arizona, USA
Field-hunting tip
Where it forms: In a vug isolated from acidic sulfate-rich solutions in the oxidized zone of a low-temperature Pb–Cu–Ag deposit. If you start seeing grandreefite, laurelite, aravaipaite in float, you are in the right ground. Typical habit: tabular crystals. Train your eye for that shape before scanning the outcrop.





