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.
Is this parthéite?
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 parthéite with a known reference. Parthéite sits at Mohs 4, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: colorless, white.
- 5Look at form & habitCrystal 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.







