Avika Natural Apophyllite Epistilbite Znco3 for Calmness/Stress reliever is one of the rarer zeolites, a popular group of minerals to collect. Satyamani Natural Apophyllite Epistilbite is crystallized, transparent mineral of the zeolite family. This mineral has a soothing quality, allows one to relieve stress and calm the spirit. Epistilbite commonly forms in the petrified bubbles (called vesicles) of volcanic rocks that have had a slight amount of exposure to metamorphism. It also forms in some pegmatites. Epistilbite\'s name means over stilbite perhaps in allusion to crystals of epistilbite that form over crystals of stilbite, a closely related zeolite. Epistilbite has similar crystal habits to stilbite although it rarely forms the large, impressive clusters that have made stilbite so famous. Satyamani Natural Apophyllite Epistilbite
DISCLAIMER: No claims are made on metaphysical properties of this stone. These literature is collected from writings, books, folklore and various sources. The actual product may slightly vary from picture as these are natural stone and no two stones can same in pattern.
Chemical Formula |
Apophyllite-KF: KCa4Si8O20(F,OH) · 8(H2O) |
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Composition |
Hydrous calcium potassium fluoro-hydroxyl-silicate. The ratio fluorine to hyroxyl varies among two group members, and the potassium is replaced with sodium in another member. |
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Variable Formula |
Apophyllite Group: (K,Na)Ca4Si8O20(F,OH) · 8(H2O) |
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Color |
Colorless, white, gray, green, brown. Rarely pink, purple, red, or orange. |
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Streak |
White |
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Hardness |
4.5 - 5 |
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Crystal System |
Tetragonal |
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Crystal Forms |
Crystals are most often in cubic-shaped crystals, with distinctive triangular corners. Commonly in perfect, pseudocubic or rectangular crystals, as well as sharply pointed prismatic pyramidal crystals that are usually doubly terminated. Also tabular, blocky, in cubic groups, in platy clusters, druzy, and instalactitic formations of crystals. An unusual habit is in blocky radiating sprays and rounded groupings resembling disco balls. Crystals are almost always striated. |
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Transparency |
Transparent to translucent |
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Specific Gravity |
2.3 - 2.4 |
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Luster |
Vitreous to greasy. Pearly on cleavage surfaces. |
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Cleavage |
1,1 |
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Fracture |
Uneven |
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Tenacity |
Brittle |
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Other ID Marks |
Occasionally fluorescent yellow or white. |
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Complex Tests |
Exfoliates and becomes fluorescent when heated. |
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In Group |
Silicates; Phyllosilicates |
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Striking Features |
Crystal habits and mode of occurrence. |
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Environment |
Mostly in volcanic rock, within basalt and in seams in diabase. Also in low temperature metamorphicveins in gneiss and in cavities in pegmatite dikes. |
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Rock Type |
Igneous |
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Popularity (1-4) |
2 |
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Prevalence (1-3) |
1 |
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Demand (1-3) |
2 |
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