Tantite is a very rare tantalum oxide mineral that typically occurs as small, platy crystals. It is primarily identified through its association with complex granite pegmatites and requires professional laboratory analysis for definitive field identification.
Is this tantite?
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 tantite with a known reference. Tantite sits at Mohs 7, 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: adamantine.
- 4Match the color rangeCompare against the expected color range: colorless.
- 5Look at form & habitCrystal system: triclinic. Typical habit: microscopic crystals.
Often confused with
Tantite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside tantite
Minerals reported to co-occur with tantite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ta₂O₅
- Mohs hardness
- 7
- Density
- 8.45 g/cm³
- Colors
- Streak
- White
- Luster
- Adamantine
- Transparency
- Transparent
- Crystal system
- Triclinic
- Crystal habit
- Microscopic crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In a granite pegmatite cutting amphibolites (Mt. Vasin-Myl’k, Russia); in a highly fractionated pegmatite (Animikie Red Ace pegmatite, Wisconsin, USA)
Where rockhounds find tantite
Classic worldwide localities
- Animikie Red Ace pegmatite, Pine River, Florence Co., Wisconsin, USA
- Mt. Vasin-Myl’k, Voron’i massif, Kola Peninsula, Russia
Field-hunting tip
Where it forms: In a granite pegmatite cutting amphibolites (Mt. Vasin-Myl’k, Russia); in a highly fractionated pegmatite (Animikie Red Ace pegmatite, Wisconsin, USA). If you start seeing microlite, stibiotantalite, holtite in float, you are in the right ground. Typical habit: microscopic crystals. Train your eye for that shape before scanning the outcrop.







