Epidote-(Sr) is a rare strontium-bearing member of the epidote group, often indistinguishable from standard epidote without chemical analysis. It typically forms in metamorphic environments where strontium-rich fluids are present, frequently occurring as small, prismatic, yellowish-brown crystals.
Is this epidote-(sr)?
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 epidote-(sr) with a known reference. Epidote-(Sr) 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. Epidote-(Sr) leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Epidote-(Sr) typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, brown, greenish-yellow.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic crystals, granular.
Often confused with
Epidote-(Sr) vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside epidote-(sr)
Minerals reported to co-occur with epidote-(sr). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaSrAl₂Fe³⁺(Si₂O₇)(SiO₄)O(OH)
- Mohs hardness
- 6-7
- Density
- 3.5-3.6 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic Crystals, Granular
- Cleavage
- Perfect in One Direction
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Metamorphic Rocks, Skarn Deposits
- Typical price
- $20-150 for rare specimen pieces
Where rockhounds find epidote-(sr)
Classic worldwide localities
- Japan
- Sweden
- Italy
Field-hunting tip
Look in metamorphic rocks, skarn deposits country — that is the host setting where epidote-(sr) typically forms. If you start seeing calcite, quartz, garnet in float, you are in the right ground. Field specimens usually show a prismatic crystals, granular habit, so train your eye for that shape before scanning the outcrop.





