Mendeleevite-(Ce) is an extremely rare and complex silicate mineral found in the alkaline pegmatites of the Lovozero Massif. Collectors prize it for its unique composition and association with other rare-earth minerals, though it is usually found as small, dark, radioactive crystal aggregates.
Is this mendeleevite-(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 mendeleevite-(ce) with a known reference. Mendeleevite-(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. Mendeleevite-(Ce) leaves a yellowish-brown streak.
- 3Read the lusterHold the specimen under a strong light. Mendeleevite-(Ce) typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: dark brown, black, reddish-brown.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: tabular crystals, aggregates.
Often confused with
Mendeleevite-(Ce) vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside mendeleevite-(ce)
Minerals reported to co-occur with mendeleevite-(ce). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- K₄Li₁₇Ca₆REE₁₆(Si₂O₇)₄(PO₄)₆O₂(OH)₃F₂
- Mohs hardness
- 5
- Density
- 4.69 g/cm³
- Streak
- Yellowish-brown
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Tabular Crystals, Aggregates
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Alkaline Pegmatites
- Typical price
- $200-800 per specimen
Where rockhounds find mendeleevite-(ce)
Classic worldwide localities
- Kola Peninsula, Russia
- Lovozero Massif, Russia
Field-hunting tip
Look in alkaline pegmatites country — that is the host setting where mendeleevite-(ce) typically forms. If you start seeing microcline, aegirine, nepheline 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.





