Irhtemite is a rare calcium-magnesium arsenate mineral known primarily from the cobalt-ore deposits of the Bou Azzer district in Morocco. It typically forms delicate, transparent tabular crystals or crusts that are often associated with other rare secondary arsenate minerals in the oxidation zone of cobalt-nickel veins.
Is this irhtemite?
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 irhtemite with a known reference. Irhtemite sits at Mohs 3, 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: silky.
- 4Match the color rangeCompare against the expected color range: white, colorless, pale rose, pink.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: spherical.
Often confused with
Irhtemite vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Streak differs, so Irhtemite leaves white, Pharmacosiderite leaves yellowish green; luster reads silky on Irhtemite and adamantine to greasy on Pharmacosiderite.

How to tell apart: Streak differs, so Irhtemite leaves white, Scorodite leaves greenish white; luster reads silky on Irhtemite and vitreous to subadamantine, subresinous on Scorodite.
Often found alongside irhtemite
Minerals reported to co-occur with irhtemite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₄Mg(AsO₄)₂(AsO₃OH)₂·4H₂O
- Mohs hardness
- 3
- Density
- 3.09 g/cm³
- Streak
- White
- Luster
- Silky
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Spherical
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Probably a dehydration product of picropharmacolite in hydrothermal ore deposits
Where rockhounds find irhtemite
Classic worldwide localities
- Irhtem (Ightem) mine, Bou Azzer district, Anti-Atlas Mountains, Morocco
- Bauhaus district, Richelsdorf Mountains, Hesse, Germany
Field-hunting tip
Where it forms: Probably a dehydration product of picropharmacolite in hydrothermal ore deposits. If you start seeing sainfeldite, erythrite in float, you are in the right ground. Typical habit: spherical. Train your eye for that shape before scanning the outcrop.


