Umbozerite is a very rare silicate mineral found in the alkaline rock complexes of the Kola Peninsula. It is highly valued by mineral collectors for its unique chemistry and radioactivity, often appearing as small, dull-brown granular masses within pegmatites.
Is this umbozerite?
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 umbozerite with a known reference. Umbozerite 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. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: bottle green, greenish brown.
- 5Look at form & habitCrystal system: amorphous. Typical habit: metamict, pseudo tetragonal.
Often confused with
Umbozerite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside umbozerite
Minerals reported to co-occur with umbozerite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₃Sr₄Th(Si₂O₇)₂(OH)₂·nH₂O
- Mohs hardness
- ~5
- Density
- 3.60 g/cm³
- Colors
- Bottle greenGreenish brown
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent to transparent
- Crystal system
- Amorphous
- Crystal habit
- Metamict, pseudo tetragonal
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In pneumatolytic-hydrothermal veins cutting alkalic rocks in the upper part of a differentiated alkalic massif
Where rockhounds find umbozerite
Classic worldwide localities
- Found on Mts. Karnasurt and Punkaruaiv, near Lake Umba, Lovozero massif, Kola Peninsula, Russia
Field-hunting tip
Where it forms: In pneumatolytic-hydrothermal veins cutting alkalic rocks in the upper part of a differentiated alkalic massif. If you start seeing ussingite, sphalerite, belovite in float, you are in the right ground. Typical habit: metamict, pseudo tetragonal. Train your eye for that shape before scanning the outcrop.






