Calcioaravaipaite is an extremely rare lead-calcium fluoride mineral typically found as tiny, delicate platy crystals in oxidized ore deposits. It is best known from the Aravaipa district in Arizona and is highly sought after by micro-mineral collectors due to its scarcity and distinct, thin tabular crystal habit.
Is this calcioaravaipaite?
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 calcioaravaipaite with a known reference. Calcioaravaipaite 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. Calcioaravaipaite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Calcioaravaipaite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: colorless, white, yellowish.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: platy crystals, thin tabular.
Often confused with
Calcioaravaipaite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside calcioaravaipaite
Minerals reported to co-occur with calcioaravaipaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- PbCa₂AlF₇(OH)₂
- Mohs hardness
- 2.5
- Density
- 6.57 g/cm³
- Streak
- White
- Luster
- Pearly
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Platy Crystals, Thin Tabular
- Cleavage
- Perfect On {001}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Lead-zinc-copper Ore Deposits
- Typical price
- $100-500 thumbnail
Where rockhounds find calcioaravaipaite
Classic worldwide localities
- Aravaipa mining district, Arizona, USA
Field-hunting tip
Look in oxidized lead-zinc-copper ore deposits country — that is the host setting where calcioaravaipaite typically forms. If you start seeing aravaipaite, wulfenite, fluorite in float, you are in the right ground. Field specimens usually show a platy crystals, thin tabular habit, so train your eye for that shape before scanning the outcrop.




