Trimerite is a rare beryllium-manganese silicate primarily known from the Långban mines and the Franklin Mining District. It is highly prized by collectors for its distinct, bright yellow-green fluorescence under ultraviolet light. It typically occurs as small, tabular crystals or massive aggregates embedded within metamorphic manganese-bearing rocks.
Is this trimerite?
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 trimerite with a known reference. Trimerite sits at Mohs 6-7, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Trimerite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Trimerite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, pink, flesh-red, brownish.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals, massive, granular.
Often confused with
Trimerite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside trimerite
Minerals reported to co-occur with trimerite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaMn²⁺BeSiO₄
- Mohs hardness
- 6-7
- Density
- 3.47 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular Crystals, Massive, Granular
- Cleavage
- Poor
- Fluorescence
- Bright Yellow-green Under SW and LW UV
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Metamorphosed Manganese Ore Deposits
- Typical price
- $100-500 per specimen
Where rockhounds find trimerite
Classic worldwide localities
- Långban, Sweden
- Franklin, New Jersey, USA
- Sterling Hill, New Jersey, USA
Field-hunting tip
Look in metamorphosed manganese ore deposits country, the host setting where trimerite typically forms. If you start seeing willemite, hardystonite, andradite in float, you are in the right ground. Field specimens usually show a tabular crystals, massive, granular habit, so train your eye for that shape before scanning the outcrop.







