Parthéite is a rare calcium-rich zeolite typically found as small, platy, or radiating crystals within hydrothermal veins. It is most easily identified by its occurrence in specific geological environments alongside other calcium-bearing zeolites and minerals like prehnite.

Hardness
4
Mohs
Luster
Vitreous
Streak
White
Transparency
Transparent

Is this parthéite?

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 parthéite with a known reference. Parthéite sits at Mohs 4, 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, white.
  • 5
    Look at form & habit
    Crystal system: monoclinic. Typical habit: fibrous, radial.

Often confused with

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

Often found alongside parthéite

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

All properties

Chemical formula
Ca₂Al₄Si₄O₁₅(OH)₂·4H₂O
Mohs hardness
4
Density
2.39-2.45 g/cm³
Streak
White
Luster
Vitreous
Transparency
Transparent
Crystal system
Monoclinic
Crystal habit
Fibrous, radial
Cleavage
{100}, {110}, distinct
Rarity
Rare
Uses
Collector
Host rock
In rodingite dikes within an ophiolite (Doģanbaba, Turkey); in veins cutting a gabbroic intrusive complex (Denezhkin Kamen complex, Russia)

Where rockhounds find parthéite

Classic worldwide localities

  • Belenköysirti Hill, seven km southeast of the village of Doģanbaba, Taurus Mountains, Burdur Province, Turkey
  • Denezhkin Kamen complex, Ural Mountains, Russia

Field-hunting tip

Where it forms: In rodingite dikes within an ophiolite (Doģanbaba, Turkey); in veins cutting a gabbroic intrusive complex (Denezhkin Kamen complex, Russia). If you start seeing prehnite, thomsonite, augite in float, you are in the right ground. Typical habit: fibrous, radial. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify parthéite?+
Mohs hardness is 4. Luster: vitreous. The streak is white. Common colors include colorless, white.
Where is parthéite found?+
Notable localities include Belenköysirti Hill, seven km southeast of the village of Doģanbaba, Taurus Mountains, Burdur Province, Turkey; Denezhkin Kamen complex, Ural Mountains, Russia.
What rocks look like parthéite?+
Parthéite is most often confused with Heulandite, Stilbite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with parthéite?+
Parthéite commonly co-occurs with Prehnite, Thomsonite, Augite, Chlorite, Tremolite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does parthéite form in?+
Where it forms: In rodingite dikes within an ophiolite (Doģanbaba, Turkey); in veins cutting a gabbroic intrusive complex (Denezhkin Kamen complex, Russia). Working float back to the host body is the standard way to chase a fresh occurrence.
What is parthéite used for?+
Parthéite is used in collector.

Find parthéite on the map

RockHoundR shows mapped rockhounding spots, access rules, and lets you log every find.

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