Magnesiocanutite is a rare hydrous manganese arsenate mineral typically occurring as small, pale yellow tabular crystals in arid environments. It is primarily found within the highly specific oxidation zones of the Torrecillas mine in Chile. Due to its extreme rarity and arsenic content, specimens are intended strictly for advanced mineral collections.
Is this magnesiocanutite?
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 magnesiocanutite with a known reference. Magnesiocanutite sits at Mohs 3-4 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Magnesiocanutite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Magnesiocanutite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, pale yellow.
- 5Look at form & habitCrystal system: triclinic. Typical habit: tabular crystals.
Often confused with
Magnesiocanutite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside magnesiocanutite
Minerals reported to co-occur with magnesiocanutite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- NaMnMn₂(AsO₄)₂·2H₂O
- Mohs hardness
- 3-4
- Density
- 3.32 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Triclinic
- Crystal habit
- Tabular Crystals
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Arid Oxidation Zones of Mineral Deposits
- Typical price
- $100-500 per specimen
Where rockhounds find magnesiocanutite
Classic worldwide localities
- Torrecillas mine, Chile
Field-hunting tip
Look in arid oxidation zones of mineral deposits country — that is the host setting where magnesiocanutite typically forms. If you start seeing gypsum, halite, thenardite in float, you are in the right ground. Field specimens usually show a tabular crystals habit, so train your eye for that shape before scanning the outcrop.





