Gasparite-(Ce) is a rare arsenic-bearing member of the monazite group, typically found as small, distinct crystals in alpine-type veins. Collectors should look for it in high-grade metamorphic environments associated with quartz and carbonate minerals. Due to its arsenic and radioactive components, it requires careful storage and handling protocols.
Is this gasparite-(ce)?
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 gasparite-(ce) with a known reference. Gasparite-(Ce) sits at Mohs 5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Gasparite-(Ce) leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Gasparite-(Ce) typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, brownish-yellow, reddish-brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: small prismatic crystals or aggregates.
Often confused with
Gasparite-(Ce) vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside gasparite-(ce)
Minerals reported to co-occur with gasparite-(ce). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CeAsO₄
- Mohs hardness
- 5
- Density
- 5.3 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Small Prismatic Crystals or Aggregates
- Cleavage
- Distinct On {100}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Veins in Metamorphic Rocks
- Typical price
- $50-300 per specimen
Where rockhounds find gasparite-(ce)
Classic worldwide localities
- Binn Valley, Switzerland
- Piz Begn, Switzerland
- Gottardo Pass, Switzerland
Field-hunting tip
Look in hydrothermal veins in metamorphic rocks country — that is the host setting where gasparite-(ce) typically forms. If you start seeing quartz, dolomite, anatase in float, you are in the right ground. Field specimens usually show a small prismatic crystals or aggregates habit, so train your eye for that shape before scanning the outcrop.





