Bityite is considered a rare mineral, and it is an endmember to the margarite mica sub-group found within the phyllosilicate group. The mineral was first described by Antoine François Alfred Lacroix in 1908, and later its chemical composition was concluded by Professor Hugo Strunz.^[5] Bityite has a close association with beryl, and it generally crystallizes in pseudomorphs after it, or in cavities associated with reformed beryl crystals.^[6] The mineral is considered a late-stage constituent in lithium bearing pegmatites,^[7] and has only been encountered in a few localities throughout the world. The mineral was named by Lacroix^[8] after Mt. Bity, Madagascar from where it was first discovered.

The first description of bityite was by Lacroix in 1908.^[8] and it was discovered on Mt. Bity, Madagascar within a pegmatite named Sahatany field [1]. It was later found in a feldspar quarry from Londonderry, Western Australia[2],^[9] and further occurrences have been found from the Middle Urals[3], and three pegmatites in Zimbabwe[4].^[10] And most recently, occurrences from the Pizzo Marcio, Val Vigezzo area in Piedmont, Italy[5] have been discovered.^[7] The most recent analysis for bityite found in the literature is for a sample from the Maantienvarsi pegmatite dyke in the Eräjärvi area in Orivesi [6], southern Finland.^[6] The sample from Maantienvarsi occurs in close association with beryl; either in cavities with altered beryl crystals, or as a pseudomorph after beryl.^[6] The mineral has been found in cavities with perthic microcline, albitic plagioclase, muscovite and tourmaline; the pseudomorphs filled with bityite have been found to contain amounts of fluorite, bertrandite, fluorapatite, quartz and beryl.^[6] The mineral substitutes into portions of beryl crystals, and is either a hydrothermal alteration product or a late stage magmatic mineral.^[7]

The current chemical formula for bityite is CaLiAl₂(AlBeSi₂)O₁₀(OH)₂.^[11] The mineral was analyzed by Lacroix, and concluded to be a new mineral rich with concentrations of lithium and beryllium.^[8] In 1947, Rowledge and Hayton discovered a new mineral from Londonderry, Western Australia with a similar chemical composition; they named it bowleyite.^[9] However, mineralogical studies performed by Strunz later confirmed that the chemical composition and properties for bowleyite were actually bityite.^[7] A recent chemical analysis found in the literature was performed with heavy liquids on a sample of bityite from the Maantienvarsi dyke to derive a computed formula for bityite based on 24 oxygens; the computed chemical formula is Ca_1.19K_0.03Na_0.02(Li_1.19Al_3.68Mg_0.35Fe_0.13)_5.35(Al_1.53Be_2.21Si_4.26)₈O_19.30(OH)_4.54F_0.16.^[6]

The samples from Mt. Bity, Maantienvarsi, and Londonderry, Western Australia show similar chemical compositions as compared to the computed composition for bityite;^[11] the chemical analysis for the three samples and the computed composition are tabulated in the adjacent table.

The atomic structure derived by X-Ray powder and optical analysis of bityite is that of a two layer modification that also exhibits a complex affinity to twinning.^[7] From studies done on mica flakes from the Maantienvarsi sample, the mineral is a two layer-type modification of polytype 2M₁.^[6] Bityite has a mica structure, shown in adjacent figure, which consists of tetrahedral and octahedral sheets separated by an interlayer cation. The mineral is considered a brittle mica, and it can be distinguished from the true micas by a layer charge per unit of approximately -2.0; in consequence, their interlayer cation is usually calcium or barium.^[12] Bityite’s structure consists of a coupled substitution it exhibits between the sheets of polyhedra; the coupled substitution of beryllium for aluminium within the tetrahedral sites allows a single lithium substitution for a vacancy without any additional octahedral substitutions.^[7] The transfer is completed by creating a tetrahedral sheet composition of Si₂BeAl.^[13] The coupled substitution of lithium for vacancy and the beryllium for the tetrahedral aluminium maintains all the charges balanced; thereby, resulting in the trioctahedral end member for the margarite sub-group of the phyllosilicate group.^[13]

Bityite exhibits a strong pearly luster, and occurs as a fine scaled white yellowish mass which is usually smaller than 0.3mm in diameter;^[6] and, its opacity is transparent to translucent.^[11] Physical properties analyses conducted with precision photographs using zirconium-filtered molybdenum radiation indicates that bityite exhibits monoclinic symmetry, and is part of the C2/c space group.^[6] The unit cell dimensions are a = 4.99 Å, b = 8.68 Å, c = 19.04 Å, β=95.17°, with a volume of 821.33 ų.^[6] The refraction indices measured by the immersion method are α = 1.650, β = 1.658, γ = 1.660 with 2V calculation of 52.9°.^[6] Bityite’s specific gravity is 3.14, and it has a hardness of 4−4.5 based on Mohs scale of hardness.^[11] Bityite’s luster is vitreous and pearly on cleavages, and it has a perfect micaceous cleavage on the {001} miller index.^[11] Bityite’s crystal habit can display thin and pseudohexagonal platy crystals.^[11]