Yanomamite is an extremely rare indium arsenate mineral found in specific hydrothermal environments. Collectors generally look for its distinctive yellow to yellow-green micro-crystalline crusts which appear in association with arsenopyrite deposits.
Is this yanomamite?
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 yanomamite with a known reference. Yanomamite sits at Mohs 3.5-4, 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: vitreous.
- 4Match the color rangeCompare against the expected color range: blue green, light green, light yellow green.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: microcrystalline crusts, tiny tabular crystals.
Often confused with
Yanomamite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside yanomamite
Minerals reported to co-occur with yanomamite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- InAsO₄·2H₂O
- Mohs hardness
- 3.5-4
- Density
- 3.87 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Semitransparent
- Crystal system
- Orthorhombic
- Crystal habit
- Microcrystalline crusts, tiny tabular crystals
- Cleavage
- Indistinct
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A rare secondary mineral replacing arsenopyrite in quartz-topaz greisen veins in granite
Where rockhounds find yanomamite
Classic worldwide localities
- Mangabeira tin deposit, near Passa e Fica, Goiás, Brazil
Field-hunting tip
Where it forms: A rare secondary mineral replacing arsenopyrite in quartz-topaz greisen veins in granite. If you start seeing scorodite, arsenopyrite, indium-rich sphalerite in float, you are in the right ground. Typical habit: microcrystalline crusts, tiny tabular crystals. Train your eye for that shape before scanning the outcrop.





