Hydroxylellestadite
A variety of Minerals
What is Hydroxylellestadite?
Fluorellestadite is a rare nesosilicate of calcium, with sulfate and fluorine, with the chemical formula Ca10(SiO4)3(SO4)3F2. It is a member of the apatite group, and forms a series with hydroxylellestadite.
Etymology & Origins
The mineral was originally named wilkeite by Eakle and Rogers in 1914, in honor of R. M. Wilke, a mineral collector and dealer. In 1922, a sample of “wilkeite” was analysed and found to be sufficiently different from the material reported by Eakle and Rogers to consider it a new species. The name “ellestadite” was proposed, in honor of Reuben B Ellestad (1900–1993), an American analytic chemist from the Laboratory for Rock Analysis, University of Minnesota, US. In 1982 Rouse and Dunn showed that the Si:S ratio was close to 1:1, giving the formula Ca10(SiO4)3(SO4)3X2, where X represents fluorine (F), hydroxyl (OH) or chlorine (Cl), and they named minerals in this group the ellestadite group. The end members of the group were named hydroxylellestadite (X = OH), fluorellestadite (X = F) and chlorellestadite (X = Cl); ideal end-member chlorellestadite is assumed not to exist in nature, although it has been synthesized. Wilkeite was discredited as a unique species, as it is not an end member of any solid solution series, but an intermediate member. The name fluorellestadite was changed to ellestadite-(F) in 2008 and changed back to fluorellestadite in 2010.
Market Value Factors
Pricing varies for every rock and mineral, so use these universal factors to gauge Hydroxylellestadite before comparing listings or appraisals.
Size & Weight
Larger, intact specimens usually command higher prices.
Rarity & Demand
Scarce material or popular varieties sell at a premium.
Condition & Finish
Chips, repairs, and heavy wear lower value; clean prep helps.
Treatment & Provenance
Untreated specimens with documented locality are prized.
Hydroxylellestadite Localities Map
See where Hydroxylellestadite is found with a localities map, collecting zones, and geology context. Generate a sample map preview below.
Key Characteristics
Characteristics of Hydroxylellestadite
Fluorellestadite shows imperfect cleavage perpendicular to the long crystal axis. The mineral is very brittle, and breaks with a conchoidal fracture. Its hardness is 4 ⁄2, between that of fluorite and apatite, and its specific gravity is 3.03 to 3.07, similar to that of fluorite. It is easily soluble in dilute hydrochloric and nitric acids and is not radioactive. When intensely heated, ellestadite (wilkeite) becomes colorless and then assumes a pale bluish green color on cooling. The mineral is uniaxial (-), with refractive indices nω = 1.638 to 1.655 and nε = 1.632 to 1.650. It is sometimes fluorescent, white to blue-white or yellow-white in short-wave ultraviolet light, and medium white-yellow-brown or weak white in long-wave light.
Appearance of Hydroxylellestadite
Fluorellestadite occurs as acicular or hexagonal prismatic, poorly terminated crystals, and as fine-grained aggregates. Crystals are transparent and aggregates are translucent. Material from Crestmore, California, is light rose-red or yellow in color, and typically occurs in a matrix of blue calcite. Material from Russia is pale bluish-green or colorless. The streak is white with a weak bluish tint, and the luster is sub-resinous on broken surfaces, but very brilliant on prism faces.
Composition of Hydroxylellestadite
The ellestadites are nesosilicates, which are minerals with isolated SiO4 tetrahedra. They are members of the apatite group, but whereas phosphorus is one of the chief constituents of apatite, in ellestadite it is almost completely replaced by sulfur and silicon, without appreciably altering the structure. The crystal class is hexagonal 6/m, space group P63/m. The tetrahedral groups are arranged to create the 63 screw axis, and the fluorine atoms are located in channels parallel to this direction. Some sources give unit cell parameters for one formula unit per unit cell (Z = 1), but some scientists consider the formula to be half the value accepted by the International Mineralogical Association (IMA), i.e. Ca5((Si,S)O4))3F, with two formula units per unit cell (Z = 2). Cell parameters for natural, as opposed to synthetic, material are a = 9.41 to 9.53 Å, and c = 6.90 to 6.94 Å. Rouse and Dunn postulated a hypothetical pure end-member with a = 9.543 Å and c = 6.917 Å. Synthetic material has a = 9.53 to 9.561 Å, and c = 6.91 to 6.920 Å.
Quick Facts
Physical Properties
- Color
- Light orange; Pink, Purple-grey
- Hardness (Mohs)
- 4.5
Chemical Properties
- Chemical Formula
- Ca5(SiO4)1.5(SO4)1.5(OH)
- Elements
- Ca, H, O, S, Si
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Hydroxylellestadite FAQs
How do I identify Hydroxylellestadite?
Hydroxylellestadite can be identified by its hardness of 4.5 on the Mohs scale, Light orange; Pink color. Look for these key characteristics when examining specimens.
What color is Hydroxylellestadite?
Hydroxylellestadite typically appears in Light orange; Pink, Purple-grey. Color can vary depending on impurities and formation conditions.
How hard is Hydroxylellestadite?
Hydroxylellestadite has a hardness of 4.5 on the Mohs scale. This gives it moderate hardness.
What is the characteristics of hydroxylellestadite of Hydroxylellestadite?
Fluorellestadite shows imperfect cleavage perpendicular to the long crystal axis. The mineral is very brittle, and breaks with a conchoidal fracture. Its hardness is 4 ⁄2, between that of fluorite and apatite, and its specific gravity is 3.03 to 3.07, similar to that of fluorite. It is easily soluble in dilute hydrochloric and nitric acids and is not radioactive. When intensely heated, ellestadite (wilkeite) becomes colorless and then assumes a pale bluish green color on cooling. The mineral is uniaxial (-), with refractive indices nω = 1.638 to 1.655 and nε = 1.632 to 1.650. It is sometimes fluorescent, white to blue-white or yellow-white in short-wave ultraviolet light, and medium white-yellow-brown or weak white in long-wave light.
What is the appearance of hydroxylellestadite of Hydroxylellestadite?
Fluorellestadite occurs as acicular or hexagonal prismatic, poorly terminated crystals, and as fine-grained aggregates. Crystals are transparent and aggregates are translucent. Material from Crestmore, California, is light rose-red or yellow in color, and typically occurs in a matrix of blue calcite. Material from Russia is pale bluish-green or colorless. The streak is white with a weak bluish tint, and the luster is sub-resinous on broken surfaces, but very brilliant on prism faces.
What is the composition of hydroxylellestadite of Hydroxylellestadite?
The ellestadites are nesosilicates, which are minerals with isolated SiO4 tetrahedra. They are members of the apatite group, but whereas phosphorus is one of the chief constituents of apatite, in ellestadite it is almost completely replaced by sulfur and silicon, without appreciably altering the structure. The crystal class is hexagonal 6/m, space group P63/m. The tetrahedral groups are arranged to create the 63 screw axis, and the fluorine atoms are located in channels parallel to this direction. Some sources give unit cell parameters for one formula unit per unit cell (Z = 1), but some scientists consider the formula to be half the value accepted by the International Mineralogical Association (IMA), i.e. Ca5((Si,S)O4))3F, with two formula units per unit cell (Z = 2). Cell parameters for natural, as opposed to synthetic, material are a = 9.41 to 9.53 Å, and c = 6.90 to 6.94 Å. Rouse and Dunn postulated a hypothetical pure end-member with a = 9.543 Å and c = 6.917 Å. Synthetic material has a = 9.53 to 9.561 Å, and c = 6.91 to 6.920 Å.
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