Thorosteenstrupine is a rare thorium-rich silicate mineral typically found in highly alkaline igneous complexes. It is closely related to the steenstrupine group and is valued primarily by advanced mineral collectors due to its distinct radioactivity and locality-specific occurrence.
Is this thorosteenstrupine?
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 thorosteenstrupine with a known reference. Thorosteenstrupine sits at Mohs 4.5-5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Thorosteenstrupine leaves a yellowish-white streak.
- 3Read the lusterHold the specimen under a strong light. Thorosteenstrupine typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: brown, yellow, reddish-brown.
- 5Look at form & habitCrystal system: trigonal. Typical habit: tabular crystals, massive, granular.
Often confused with
Thorosteenstrupine vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside thorosteenstrupine
Minerals reported to co-occur with thorosteenstrupine. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Ca,Th,Mn)₂(Si,P,Al)₄O₁₁(OH,F)₂·nH₂O
- Mohs hardness
- 4.5-5
- Density
- 3.3-3.6 g/cm³
- Colors
- Streak
- Yellowish-white
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Trigonal
- Crystal habit
- Tabular Crystals, Massive, Granular
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Alkaline Pegmatites
- Typical price
- $50-300 per specimen depending on size and quality
Where rockhounds find thorosteenstrupine
Classic worldwide localities
- Ilimaussaq Complex, Greenland
- Kola Peninsula, Russia
Field-hunting tip
Look in alkaline pegmatites country — that is the host setting where thorosteenstrupine typically forms. If you start seeing eudialyte, microcline, aegirine in float, you are in the right ground. Field specimens usually show a tabular crystals, massive, granular habit, so train your eye for that shape before scanning the outcrop.





