Merwinite is a rare nesosilicate mineral typically found in high-temperature contact metamorphic zones where limestones have been altered by igneous intrusions. It most commonly appears as colorless or pale green granular masses rather than well-defined crystals. It is a prized specimen for advanced collectors specializing in skarn mineralogy.
Is this merwinite?
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 merwinite with a known reference. Merwinite sits at Mohs 6, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Merwinite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Merwinite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white, pale green, gray.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: granular, massive, or as rare small prismatic crystals.
Often confused with
Merwinite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside merwinite
Minerals reported to co-occur with merwinite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₃Mg(SiO₄)₂
- Mohs hardness
- 6
- Density
- 3.15-3.20 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Granular, Massive, Or as Rare Small Prismatic Crystals
- Cleavage
- Poor
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Contact Metamorphosed Limestone (skarn Deposits)
- Typical price
- $20-100 per specimen
Where rockhounds find merwinite
Classic worldwide localities
- Crestmore, California, USA
- Carlingford, Ireland
- Kilchoan, Scotland
- Fuka, Japan
Field-hunting tip
Look in contact metamorphosed limestone (skarn deposits) country, the host setting where merwinite typically forms. If you start seeing larnite, gehlenite, calcite in float, you are in the right ground. Field specimens usually show a granular, massive, or as rare small prismatic crystals habit, so train your eye for that shape before scanning the outcrop.





