Ardealite is a rare phosphate-sulfate mineral that typically forms through the reaction of bat guano with limestone bedrock in cave environments. It is most commonly found as earthy, white to yellowish massive coatings or crusts and is often visually indistinguishable from related phosphate minerals without laboratory analysis.
Is this ardealite?
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 ardealite with a known reference. Ardealite sits at Mohs 2 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Ardealite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Ardealite typically shows a dull luster.
- 4Match the color rangeCompare against the expected color range: white, yellowish-white, pale yellow.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: massive, earthy, or powdery crusts.
Often confused with
Ardealite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside ardealite
Minerals reported to co-occur with ardealite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₂(SO₄)(HPO₄)·4H₂O
- Mohs hardness
- 2
- Density
- 2.44 g/cm³
- Streak
- White
- Luster
- Dull
- Transparency
- Opaque
- Crystal system
- Monoclinic
- Crystal habit
- Massive, Earthy, Or Powdery Crusts
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Bat Guano Deposits in Limestone Caves
- Typical price
- $20-100 per specimen
Where rockhounds find ardealite
Classic worldwide localities
- Cioclovina Cave, Romania
- various guano-rich cave deposits worldwide
Field-hunting tip
Look in bat guano deposits in limestone caves country — that is the host setting where ardealite typically forms. If you start seeing brushite, gypsum, hydroxyapatite in float, you are in the right ground. Field specimens usually show a massive, earthy, or powdery crusts habit, so train your eye for that shape before scanning the outcrop.


