Paraniite-(Y) is a rare calcium yttrium arsenate that forms creamy yellow rough crystals. It was approved as a distinct mineral species in 1992. It was first described from the east flank of Pizzo Cervandone, Alpe Devero, Valle d'Ossola, Piedmont, Italy.
Is this paraniite-(y)?
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 paraniite-(y) with a known reference. Paraniite-(Y) sits at Mohs 3-4, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Paraniite-(Y) leaves a yellowish-white streak.
- 3Read the lusterHold the specimen under a strong light. Paraniite-(Y) typically shows a vitreous to adamantine luster.
- 4Match the color rangeCompare against the expected color range: creamy yellow.
- 5Look at form & habitCrystal system: tetragonal. Typical habit: rough crystals.
Often confused with
Paraniite-(Y) vs. its common look-alikes, and how to tell them apart in the field.
How to tell apart: Streak differs, so Paraniite-(Y) leaves yellowish-white, Tundrite-(Nd) leaves white; luster reads vitreous to adamantine on Paraniite-(Y) and vitreous on Tundrite-(Nd).

How to tell apart: Stillwellite-(Ce) is the harder of the two (Mohs 6.5 vs. 3-4); streak differs, so Paraniite-(Y) leaves yellowish-white, Stillwellite-(Ce) leaves white; luster reads vitreous to adamantine on Paraniite-(Y) and vitreous on Stillwellite-(Ce).
Often found alongside paraniite-(y)
Minerals reported to co-occur with paraniite-(y). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₂Y(WO₄)₂(AsO₄)
- Mohs hardness
- 3-4
- Density
- 5.95 g/cm³
- Colors
- Streak
- Yellowish-white
- Luster
- Vitreous to Adamantine
- Transparency
- Translucent
- Crystal system
- Tetragonal
- Crystal habit
- Rough Crystals
- Cleavage
- On {001}, Distinct
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Alkaline Pegmatites
Where rockhounds find paraniite-(y)
Classic worldwide localities
- east flank of Pizzo Cervandone, Piedmont, Italy
Field-hunting tip
Look in alkaline pegmatites country, the host setting where paraniite-(y) typically forms. If you start seeing quartz, microcline, biotite in float, you are in the right ground. Field specimens usually show a rough crystals habit, so train your eye for that shape before scanning the outcrop.




