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. Metatamboite leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Metatamboite typically shows a adamantine luster.
- 4Match the color rangeCompare against the expected color range: yellow, yellow-orange, brown.
- 5Look at form & habitCrystal system: orthorhombic. 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
- Pb₄(TeO₃)₃(SO₄)
- Mohs hardness
- 2-3
- Density
- 6.05 g/cm³
- Colors
- Streak
- Yellow
- Luster
- Adamantine
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Platy Crystals, Tabular, Micaceous Aggregates
- Cleavage
- Perfect in One Direction
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Tellurium-bearing Hydrothermal Ore Deposits
- Typical price
- $100-500 per specimen depending on size and quality
Where rockhounds find metatamboite
Classic worldwide localities
- Moctezuma mine, Sonora, Mexico
- Tombstone, Arizona, USA
Field-hunting tip
Look in oxidized tellurium-bearing hydrothermal ore deposits country — that is the host setting where metatamboite typically forms. If you start seeing tellurite, emmonsite, paratellurite in float, you are in the right ground. Field specimens usually show a platy crystals, tabular, micaceous aggregates habit, so train your eye for that shape before scanning the outcrop.




