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.

Hardness
6.5-7
Mohs
Luster
Pitch-like to vitreous
Streak
Gray-greenish
Transparency
Translucent

Is this dissakisite-(la)?

5-step field check

Run through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.

  • 1
    Test the hardness
    Try to scratch dissakisite-(la) with a known reference. Dissakisite-(La) sits at Mohs 6.5-7, softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Streak: gray-greenish.
  • 3
    Read the luster
    Hold the specimen under a strong light. Luster: pitch-like to vitreous.
  • 4
    Match the color range
    Compare against the expected color range: black, very dark brown.
  • 5
    Look at form & habit
    Crystal system: monoclinic. Typical habit: aggregates, anhedral grains, inclusions.

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
CaLaMgAl₂(Si₂O₇)(SiO₄)O(OH)
Mohs hardness
6.5-7
Density
3.79 g/cm³
Colors
BlackVery dark brown
Streak
Gray-greenish
Luster
Pitch-like to vitreous
Transparency
Translucent
Crystal system
Monoclinic
Crystal habit
Aggregates, anhedral grains, inclusions
Cleavage
Imperfect on (001)
Rarity
Rare
Uses
Collector, Scientific research
Host rock
By hydration and enrichment in LILE and LREE of a garnet-bearing peridotite body, in relation to HP-migmatization of the surrounding gneisses during an orogeny

Where rockhounds find dissakisite-(la)

Classic worldwide localities

  • Japan
  • Norway
  • Italy
  • United States

Field-hunting tip

Where it forms: By hydration and enrichment in LILE and LREE of a garnet-bearing peridotite body, in relation to HP-migmatization of the surrounding gneisses during an orogeny. If you start seeing olivine, spinel, amphiboles in float, you are in the right ground. Typical habit: aggregates, anhedral grains, inclusions. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify dissakisite-(la)?+
Mohs hardness is 6.5-7. Luster: pitch-like to vitreous. The streak is gray-greenish. Common colors include black, very dark brown.
Where is dissakisite-(la) found?+
Notable localities include Japan; Norway; Italy; United States.
Is dissakisite-(la) safe to handle?+
Dissakisite-(La) contains trace uranium or thorium. Wash your hands afterwards, never grind or breathe the dust, and store it apart from specimens you handle often.
What rocks look like dissakisite-(la)?+
Dissakisite-(La) is most often confused with Epidote, Allanite-(Ce), Clinozoisite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with dissakisite-(la)?+
Dissakisite-(La) commonly co-occurs with Olivine, Spinel, Amphiboles, Clino- and orthopyroxenes, Clinochlore, Uraninite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does dissakisite-(la) form in?+
Where it forms: By hydration and enrichment in LILE and LREE of a garnet-bearing peridotite body, in relation to HP-migmatization of the surrounding gneisses during an orogeny. Working float back to the host body is the standard way to chase a fresh occurrence.
What is dissakisite-(la) used for?+
Dissakisite-(La) is used in collector, scientific research.

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