Ellenbergerite is an extremely rare silicate mineral found in ultra-high-pressure metamorphic rocks. It typically occurs as small, pale pink or colorless prismatic crystals, primarily recognized from its type locality in the Dora-Maira massif of Italy.

Hardness
6.5
Mohs
Luster
Vitreous
Streak
White
Transparency
Transparent

Is this ellenbergerite?

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 ellenbergerite with a known reference. Ellenbergerite sits at Mohs 6.5, softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Streak: white.
  • 3
    Read the luster
    Hold the specimen under a strong light. Luster: vitreous.
  • 4
    Match the color range
    Compare against the expected color range: colorless, purple, lilac.
  • 5
    Look at form & habit
    Crystal system: hexagonal. Typical habit: hexagonal prismatic crystals.

Often confused with

Ellenbergerite vs. its common look-alikes, and how to tell them apart in the field.

Often found alongside ellenbergerite

Minerals reported to co-occur with ellenbergerite. Spotting these in float or country rock is a strong cue you are in the right ground.

All properties

Chemical formula
Mg₆(Mg,Ti,Zr,□)₂(Al,Mg)₆Si₈O₂₈(OH)₁₀
Mohs hardness
6.5
Density
3.15-3.22 g/cm³
Colors
Streak
White
Luster
Vitreous
Transparency
Transparent
Crystal system
Hexagonal
Crystal habit
Hexagonal prismatic crystals
Cleavage
None
Rarity
Rare
Uses
Collector
Host rock
As inclusions in pyrope porphyroblasts developed during high-pressure (25–30 kbar), medium-temperature (700 ° C{800 ° C) metamorphism of continental crustal rocks

Where rockhounds find ellenbergerite

Classic worldwide localities

  • Dora-Maira massif, Parigi, near Martiniana Po, Piedmont, Italy

Field-hunting tip

Where it forms: As inclusions in pyrope porphyroblasts developed during high-pressure (25–30 kbar), medium-temperature (700 ° C{800 ° C) metamorphism of continental crustal rocks. If you start seeing pyrope, kyanite, talc in float, you are in the right ground. Typical habit: hexagonal prismatic crystals. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify ellenbergerite?+
Mohs hardness is 6.5. Luster: vitreous. The streak is white. Common colors include colorless, purple, lilac.
Where is ellenbergerite found?+
Notable localities include Dora-Maira massif, Parigi, near Martiniana Po, Piedmont, Italy.
What rocks look like ellenbergerite?+
Ellenbergerite is most often confused with Quartz, Phenakite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with ellenbergerite?+
Ellenbergerite commonly co-occurs with Pyrope, Kyanite, Talc, Clinochlore, Rutile, Zircon. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does ellenbergerite form in?+
Where it forms: As inclusions in pyrope porphyroblasts developed during high-pressure (25–30 kbar), medium-temperature (700 ° C{800 ° C) metamorphism of continental crustal rocks. Working float back to the host body is the standard way to chase a fresh occurrence.
What is ellenbergerite used for?+
Ellenbergerite is used in collector.

Find ellenbergerite on the map

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