Thortveitite is a rare scandium-rich silicate mineral primarily found in granitic pegmatites. It typically occurs as elongated, gray-green prisms and is highly prized by mineral collectors as the primary industrial source of scandium.
Is this thortveitite?
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 thortveitite with a known reference. Thortveitite sits at Mohs 6-7, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Thortveitite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Thortveitite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: grayish-green, gray, greenish-white.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic crystals, often elongated and striated.
Often confused with
Thortveitite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside thortveitite
Minerals reported to co-occur with thortveitite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Sc,Y)₂Si₂O₇
- Mohs hardness
- 6-7
- Density
- 3.27-3.43 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic Crystals, Often Elongated and Striated
- Cleavage
- Distinct
- Rarity
- Rare
- Uses
- Collector, Source of Scandium
- Host rock
- Granite Pegmatites
- Typical price
- $100-500 thumbnail, $500+ specimen grade
Where rockhounds find thortveitite
Classic worldwide localities
- Iveland, Norway
- Madagascar
- Hittero, Norway
- Arizona, USA
- New Mexico, USA
Field-hunting tip
Look in granite pegmatites country, the host setting where thortveitite typically forms. If you start seeing microcline, beryl, monazite in float, you are in the right ground. Field specimens usually show a prismatic crystals, often elongated and striated habit, so train your eye for that shape before scanning the outcrop.






