Kristiansenite is an exceptionally rare scandium-bearing phosphate mineral found in alkaline syenite pegmatites. It typically occurs as small, colorless tabular crystals or crystalline aggregates associated with other rare earth minerals in the Larvik Plutonic Complex of Norway.
Is this kristiansenite?
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 kristiansenite with a known reference. Kristiansenite sits at Mohs 3.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Kristiansenite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Kristiansenite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white.
- 5Look at form & habitCrystal system: triclinic. Typical habit: tabular crystals, aggregates.
Often confused with
Kristiansenite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside kristiansenite
Minerals reported to co-occur with kristiansenite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaSc(PO₄)F₂
- Mohs hardness
- 3.5
- Density
- 2.98 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Triclinic
- Crystal habit
- Tabular Crystals, Aggregates
- Cleavage
- Perfect in One Direction
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Syenite Pegmatites
- Typical price
- $100-500+ for micro-specimens
Where rockhounds find kristiansenite
Classic worldwide localities
- Tvedalen, Larvik, Norway
Field-hunting tip
Look in syenite pegmatites country — that is the host setting where kristiansenite typically forms. If you start seeing albite, aegirine, microcline in float, you are in the right ground. Field specimens usually show a tabular crystals, aggregates habit, so train your eye for that shape before scanning the outcrop.







