Metatamboite is a rare secondary tellurite mineral typically occurring as fragile, platy or micaceous crystals in oxidized zones of tellurium-rich ore bodies. It is most easily identified by its distinctive yellow to brownish-orange color and association with other secondary tellurium minerals in specific localities like the Moctezuma mine.
Is this metatamboite?
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 metatamboite with a known reference. Metatamboite sits at Mohs 2-3, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: very pale yellow to colorless.
- 3Read the lusterHold the specimen under a strong light. Luster: greasy to vitreous.
- 4Match the color rangeCompare against the expected color range: pale yellow.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: platy crystals, tabular, micaceous aggregates.
Often confused with
Metatamboite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside metatamboite
Minerals reported to co-occur with metatamboite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Fe₃(OH)(H₂O)₂(SO₄)(TeO₃)₃(TeO(OH)₂)(H₂O)
- Mohs hardness
- 2-3
- Density
- 4.053 g/cm³
- Colors
- Streak
- Very pale yellow to colorless
- Luster
- Greasy to vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Platy crystals, tabular, micaceous aggregates
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In the interstices of silicified epithermal hydrothermal breccias of dacitic tuff
Where rockhounds find metatamboite
Classic worldwide localities
- Moctezuma mine, Sonora, Mexico
- Tombstone, Arizona, USA
Field-hunting tip
Where it forms: In the interstices of silicified epithermal hydrothermal breccias of dacitic tuff. If you start seeing alunite, rodalquilarite, emmonsite in float, you are in the right ground. Typical habit: platy crystals, tabular, micaceous aggregates. Train your eye for that shape before scanning the outcrop.







