Kamphaugite-(Y) is a rare yttrium-bearing carbonate mineral that typically occurs as thin, platy, pearl-like crystals. It is primarily found in complex rare-earth element (REE) environments associated with syenite pegmatites. Collectors generally look for its characteristic radial or rosette-like crystal clusters in hydrothermal vugs.
Is this kamphaugite-(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 kamphaugite-(y) with a known reference. Kamphaugite-(Y) sits at Mohs 2-3, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: white, brown, colorless, light yellow.
- 5Look at form & habitCrystal system: tetragonal. Typical habit: spherical.
Often confused with
Kamphaugite-(Y) vs. its common look-alikes, and how to tell them apart in the field.
All properties
- Chemical formula
- CaY(CO₃)₂(OH)·H₂O
- Mohs hardness
- 2-3
- Density
- 3.19 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent to translucent
- Crystal system
- Tetragonal
- Crystal habit
- Spherical
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A late, low-temperature mineral formed in a contact-metamorphic skarn (Hørtekollen deposit, Norway); in metasomatically altered alkali granite (Kazakhstan)
Where rockhounds find kamphaugite-(y)
Classic worldwide localities
- Gronci-Ellis granite quarry, Mount Desert, Hancock Co., Maine, USA
- Hørtekollen deposit, Lier, Buskerud, Norway
- Høydalen granite pegmatite, Tørdal, Telemark, Norway
- Tangen granite pegmatite, near Kragerø, Norway
- Cala Francese, Sardinia, Italy
- Szarvaskő, Bükk Mountains, Hungary
Field-hunting tip
Where it forms: A late, low-temperature mineral formed in a contact-metamorphic skarn (Hørtekollen deposit, Norway); in metasomatically altered alkali granite (Kazakhstan). If you start seeing kuliokite-, gagarinite, kainosite- in float, you are in the right ground. Typical habit: spherical. Train your eye for that shape before scanning the outcrop.

