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. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: colorless, gray, pale green.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: granular.
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
- 3.15-3.32 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent to translucent
- Crystal system
- Monoclinic
- Crystal habit
- Granular
- Cleavage
- Perfect on {100}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In siliceous dolomitic limestone in contact metamorphic zones, formed at relatively elevated temperatures, locally in substantial quantities
Where rockhounds find merwinite
Classic worldwide localities
- Crestmore, Riverside Co., California, USA
- Neihart, Cascade Co., Montana, USA
- Christmas Mountains, Brewster Co., Texas, USA
- Velardeña, Durango, Mexico
- Scawt Hill, near Larne, Co. Antrim, Ireland
- Found near Anakit Creek, at the mouth of the Lower Tunguska River, central Siberia, and in the Ozerskii massif, Lake Baikal, Russia
Field-hunting tip
Where it forms: In siliceous dolomitic limestone in contact metamorphic zones, formed at relatively elevated temperatures, locally in substantial quantities. If you start seeing gehlenite, spurrite, monticellite in float, you are in the right ground. Typical habit: granular. Train your eye for that shape before scanning the outcrop.






