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. Irhtemite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Irhtemite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: white, colorless, pinkish.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals, crusts, radial aggregates.
Often confused with
Irhtemite vs. its common look-alikes — and how to tell them apart in the field.
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
- 3.37 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular Crystals, Crusts, Radial Aggregates
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Cobalt-nickel-arsenic Veins
- Typical price
- $50-300 per specimen
Where rockhounds find irhtemite
Classic worldwide localities
- Bou Azzer, Morocco
Field-hunting tip
Look in hydrothermal cobalt-nickel-arsenic veins country — that is the host setting where irhtemite typically forms. If you start seeing arsenolite, picropharmacolite, fluckite in float, you are in the right ground. Field specimens usually show a tabular crystals, crusts, radial aggregates habit, so train your eye for that shape before scanning the outcrop.






