Skarn is a metasomatic rock formed through the interaction of hot hydrothermal fluids with carbonate-rich rocks like limestone or dolostone. Collectors prize skarns for their diverse and often showy mineral assemblages, which frequently include large crystals of garnet, pyroxene, and epidote.
Is this skarn?
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 skarn with a known reference. Skarn sits at Mohs 5-7, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Skarn leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Skarn typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: green, brown, black, white, red.
- 5Look at form & habitTypical habit: massive.
Often found alongside skarn
Minerals reported to co-occur with skarn. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Mohs hardness
- 5-7
- Density
- 2.8-3.6 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal habit
- Massive
- Cleavage
- None
- Rarity
- Common
- Uses
- Collector, Industrial
- Host rock
- Metasomatized Carbonate Rocks
- Typical price
- $5-50 for small specimens, higher for specific mineral associations
Where rockhounds find skarn
Classic worldwide localities
- Sweden
- USA
- Mexico
- Russia
- China
Field-hunting tip
Look in metasomatized carbonate rocks country, the host setting where skarn typically forms. If you start seeing garnet, pyroxene, epidote in float, you are in the right ground. Field specimens usually show a massive habit, so train your eye for that shape before scanning the outcrop.





