Dollaseite-(Ce) is a rare member of the epidote group, typically occurring as prismatic or tabular crystals in magnesium-rich skarn environments. Collectors should look for its distinct brownish coloration and close association with calcium-silicate minerals in contact metamorphic zones.
Is this dollaseite-(ce)?
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 dollaseite-(ce) with a known reference. Dollaseite-(Ce) sits at Mohs 6-6.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Dollaseite-(Ce) leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Dollaseite-(Ce) typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: brown, reddish-brown, dark brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic to tabular crystals, often in radial aggregates.
Often confused with
Dollaseite-(Ce) vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside dollaseite-(ce)
Minerals reported to co-occur with dollaseite-(ce). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaCeMgAlFe²⁺Si₃O₁₂OH
- Mohs hardness
- 6-6.5
- Density
- 3.8-4.0 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic to Tabular Crystals, Often in Radial Aggregates
- Cleavage
- Poor
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Skarn Deposits and Carbonate Rocks
- Typical price
- $50-300 per specimen depending on size and quality
Where rockhounds find dollaseite-(ce)
Classic worldwide localities
- Sweden
- USA
- Japan
Field-hunting tip
Look in skarn deposits and carbonate rocks country — that is the host setting where dollaseite-(ce) typically forms. If you start seeing calcite, diopside, garnet in float, you are in the right ground. Field specimens usually show a prismatic to tabular crystals, often in radial aggregates habit, so train your eye for that shape before scanning the outcrop.







