Dissakisite-(La) is a rare lanthanum-dominant member of the epidote group, often occurring as small, dark, prismatic crystals in metamorphic environments. It is visually indistinguishable from other allanite-group minerals in the field and typically requires chemical analysis for definitive identification. Collectors often seek it out for its significance as a rare earth element-bearing mineral species.
Is this dissakisite-(la)?
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 dissakisite-(la) with a known reference. Dissakisite-(La) 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. Dissakisite-(La) leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Dissakisite-(La) typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: black, brown, dark brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic crystals.
Often confused with
Dissakisite-(La) vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside dissakisite-(la)
Minerals reported to co-occur with dissakisite-(la). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaLaAl₂Fe²⁺(Si₂O₇)(SiO₄)O(OH)
- Mohs hardness
- 6-7
- Density
- 3.5-3.6 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic Crystals
- Cleavage
- Good in One Direction
- Rarity
- Rare
- Uses
- Collector, Scientific Research
- Host rock
- Metamorphic Rocks
- Typical price
- $50-500 depending on crystal quality and size
Where rockhounds find dissakisite-(la)
Classic worldwide localities
- Japan
- Norway
- Italy
- United States
Field-hunting tip
Look in metamorphic rocks country — that is the host setting where dissakisite-(la) typically forms. If you start seeing quartz, feldspar, garnet in float, you are in the right ground. Field specimens usually show a prismatic crystals habit, so train your eye for that shape before scanning the outcrop.







