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Formula | (Na,K,Ca0.5,Sr0.5,Ba0.5,Mg0.5)6Al6Si30O72 ∙ 20H2O |
| Optic class & sign | Biaxial positive or negative |
| Optical orientation | X = b, Y near a, Z near c |
| Optical plane | Optic plane ⊥ (010l) |
| Relief | Moderate-negative |
| Refractive indices | nx = 1.473 -1.491
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ny = 1.475 -1.493
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nz = 1.478 -1.497
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n increases with CaAl substituting for NaSi |
| Birefringence (max.) | 0.003 - 0.006 |
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| Optic Angle
| 2Vx
= 85 - 90° |
| 2Vz
= 90 - 32° |
| Sign of elongation | Length-slow, l (+), for elongate cross-sections ⊥ (010), for the optical orientation shown; other indicatrix orientations show length-fast, I (-) |
| Interference figure | |
| Colour / pleochroism | Colourless |
| Zoning | - |
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Form | Habit | Platy |
| | Surface | |
| Cleavage | {010} |
| Twinning | Commonly not twinned |
| Extinction | Z∧c or trace of {100} = 18 – 23°; higher for K-Cpt |
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Reaction textures | |
| Alteration / decomposition | |
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Occurence | Ign | |
| | Met | Sediments incl pyroclastics at lowest-grade burial metamorphism, also from devitrification |
| | Sed | Diagenetic in submarine sediments, lake deposits |
| | Hyd | Cavities and veins in basalt, andesite and rhyolite |
| | Other | |
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Distinctive properties | Common zeolite. Very low n, very low to low Δn. Heulandite and clinoptilolite are difficult to distinguish from each other, but heulandite has commonly higher refractive indices. |
| Additional comments | n-Δn charts A, B: Bre - brewsterite, Cpt - clinoptilolite, Epi - epistilbite, Hul - heulandite, Lev - levyne, Stb - stilbite, Yug - yugawaralite |
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