Hilgardite

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Hilgardite
Hilgardite-Boracite-180073.jpg
Microcrystalline red-orange hilgardite encasing white boracite, from Boulby Mine, Loftus, North Yorkshire, England. Size: 5.5 × 4.5 × 3.4 cm.
General
CategoryTektoborates
Formula
(repeating unit)
Ca2B5O9Cl·H2O
IMA symbolHgr[1]
Strunz classification6.ED.05
Crystal systemTriclinic
Crystal classPedial (1)
(same H-M symbol)
Space groupP1
Unit cella = 6.297, b = 6.464
c = 6.565 [Å]; α = 74.24°
β = 61.68°, γ = 61.26°; Z = 1
Identification
ColorColorless, light pink to reddish brown
Crystal habitTabular triangular crystals
Cleavage{010}, perfect; {100}, good
FractureConchoidal
Mohs scale hardness5
LusterVitreous
StreakWhite
DiaphaneityTransparent to translucent
Specific gravity2.67–2.71
Optical propertiesBiaxial (+)
Refractive indexnα = 1.630 nβ = 1.636 nγ = 1.664
Birefringenceδ = 0.034
2V angleMeasured: 35°
Other characteristicsPiezoelectric
References[2][3][4]

Hilgardite is a borate mineral with the chemical formula Ca2B5O9Cl·H2O. It is transparent and has vitreous luster. It is colorless to light pink with a white streak. It is rated 5 on the Mohs Scale. It crystallizes in the triclinic crystal system. Crystals occur as distorted tabular triangles and are hemimorphic, polytypes exist.[2][3]

It was named for geologist Eugene W. Hilgard (1833–1916). It was first described in 1937 for an occurrence in the Choctaw Salt Dome of Iberville Parish, Louisiana, US.[2] It occurs as an uncommon accessory mineral in evaporite deposits and salt domes worldwide. In addition to the type locality it has been reported in Wayne County, Mississippi and in the Louann Salt Formation, Clarke County, Alabama in the United States and at the Penobsquis and Salt Springs evaporites, near Sussex, New Brunswick, Canada. In Europe it is reported from the Konigshall-Hindenburg potash mine near Göttingen, Lower Saxony, Germany and in the Boulby potash mine, Whitby, Yorkshire, England. In Asia it is reported from the Chelkar salt dome, Uralsk district, Kazakhstan; the Ilga Basin, eastern Siberia, Russia and the Sedom Formation, Mount Sedom, Dead Sea, Israel.[2][3]

See also[]

References[]

  1. ^ Warr, L.N. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine. 85 (3): 291–320. Bibcode:2021MinM...85..291W. doi:10.1180/mgm.2021.43. S2CID 235729616.
  2. ^ a b c d Mindat.org
  3. ^ a b c Handbook of Mineralogy
  4. ^ Webmineral data
  • S. Ghose and C. Wan, Hilgardite, Ca2[B5O9]Cl·H2O; a piezoelectric zeolite-type pentaborate, American Mineralogist; February 1979; v. 64; no. 1-2; p. 187-195
  • Burns, P. C. and F. C. Hawthorne, Refinement of the structure of Hilgardite-1A, Acta crystallographica. Section C, 1994, vol. 50 (5), pp. 653–655
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