Piergorite-(Ce) is a rare silicate mineral found in alkaline pegmatite environments. It typically forms small prismatic crystals and is recognized by its distinct brown to yellow coloration and characteristic association with rare earth element minerals.
Is this piergorite-(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 piergorite-(ce) with a known reference. Piergorite-(Ce) sits at Mohs 5.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Piergorite-(Ce) leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Piergorite-(Ce) typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, brown, dark brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic crystals.
Often confused with
Piergorite-(Ce) vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside piergorite-(ce)
Minerals reported to co-occur with piergorite-(ce). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaCe₄(Si₂O₇)(SiO₄)O(OH)₃
- Mohs hardness
- 5.5
- Density
- 4.15 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Alkaline Pegmatites
- Typical price
- $50-300 per specimen
Where rockhounds find piergorite-(ce)
Classic worldwide localities
- Kola Peninsula, Russia
- Srednyaya Varaka, Russia
Field-hunting tip
Look in alkaline pegmatites country — that is the host setting where piergorite-(ce) typically forms. If you start seeing apatite, quartz, titanite in float, you are in the right ground. Field specimens usually show a prismatic crystals habit, so train your eye for that shape before scanning the outcrop.





