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 — that is 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.





