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| Lithosite |
K3 [HAl2Si4O13]
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| Morphology: |
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Irregular
grains 1-3 mm in size.
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| Physical
properties: |
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Hardness: 5½ on Mohs scale
Density = 2.51 gm/cm3(Measured) 2.54 gm/cm3(Calculated)
Luster: vitreous
Streak: White
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| Optical properties: |
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Color: Colorless; bright pink
after X-ray irradiation for at least 8 months. Biaxial (+)
α = 1.510(2) , β = 1.513(2), γ = 1.527(2); 2V: Measured: 47° ,
Calculated: 52°
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Colorless crystals of lithosite from Vuonnemiok River Valley,
Khibiny Massif, Murmansk Oblast, Russia.
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| Crystallography: |
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Unit cell: a 15.197, b
10.233, c 8.435 Ε, β 90.21°
Z = 2. Space group: n.d.
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| Name: |
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The name is from the Greek lithos meaning stone, because it is
composed of the most abundant components in the Earth's crust.
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| Crystal structure: |
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The framework topology of the –LIT zeolite consists of three
types of secondary building units of 6 or 4-[1,1] or 4-2 and
includes four, six, and eight-membered rings (4, 6, 8MR) of
tetrahedral atoms. It is characteristic of this topology to
include a pseudo 10MR accompanied by terminal silanol groups. The
–LIT type structure has a three-dimensional pore structure, and
8MR contacts pseudo 10MR. Potassium cations are densely
accommodated in micropores.

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The framework of lithosite, with Si/Al framework in beige,O atoms
in red and K atoms in purple.
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| Chemical composition: |
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Electron microprobe analysis of a sample from Khibiny massif,
Russia corresponds to K5.84Al3.94Si 8.08O25
· 2.5H2O.
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| Occurrences: |
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Lithosite is a natural zeolite that was first discovered in
Vuonnemiok River Valley, Khibiny Massif, Murmansk Oblast, Russia.
Occurs in veins of ultra-agpaitic pegmatite cutting nepheline
syenites (rischorrites). Standard samples are preserved in the
Fersman Mineralogical Museum, USSR Academy of Sciences, and the
Museum of the Geological Institute of the Kola Branch, USSR
Academy of Sciences.
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| References: |
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Khomyakov, A. P., Chernitsova, N. M., and Chistyakova, N. I.
(1983) Lithosite K6Al4Si8O25·
2H2O — a new mineral. International Geology Review,
25(6), 741-744.
Pudovkina, Z. V., Solov'eva, L. P., and Pyatenko, Y. A. (1986).
Crystal structure of lithosite K3[HAl2Si4O13].
In Soviet Physics Doklady (Vol. 31, p. 941).
Updated: May 2025.
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