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Wardite

Hydrated phosphate mineral


Hydrated phosphate mineral

FieldValue
nameWardite
imageWardite.jpg
captionWardite from Rapid Creek – Yukon, Canada
categoryPhosphate minerals
formulaNaAl3(PO4)2(OH)4·2(H2O)
IMAsymbolWd
strunz8.DL.10
systemTetragonal
classTrapezohedral (422)
H-M symbol: (4 2 2)
symmetry*P*41212
unit cella = 7.03(1), c = 19.04(1) Å;
Z = 4
colorWhite, colorless, pale green, blue-green, yellow-green, pale yellow, yellow pink.
habitDipyramidal pseudo-octahedral crystals, striated; radial, fibrous, encrustations
cleavagePerfect on {001}
mohs5
lusterVitreous
diaphaneityTransparent to opaque
gravity2.81–2.87
opticalpropUniaxial (+)
refractivenω = 1.586 – 1.594 nε = 1.595 – 1.604
birefringenceδ = 0.009
2V0.0
references

H-M symbol: (4 2 2) Z = 4 | length fast/slow =

Wardite is a hydrous sodium aluminium phosphate hydroxide mineral with formula: NaAl3(PO4)2(OH)4·2(H2O). Wardite is of interest for its rare crystallography. It crystallizes in the tetragonal trapezohedral class and is one of only a few minerals in that class. Wardite forms vitreous green to bluish green to white to colorless crystals, with pyramidal {102} or {114} faces and with {001} usually present masses. Also appears as fibrous encrustations. It has a Mohs hardness of 5 and a specific gravity of 2.81–2.87.

Wardite was named for Henry Augustus Ward (1834–1906) of the University of Rochester in New York. It first described in 1896 for an occurrence in Clay Canyon, Fairfield, Utah County, Utah, US.

Occurrence

It occurs with variscite in phosphate nodules and occurs uncommonly in pegmatites and phosphate deposits through alteration of amblygonite.

Wardite is a rare mineral, which has been found in approximately 70 locations worldwide, but generally on a microscopic scale, with only a few occurrences of significant specimens. The finest specimens, boasting crystals up to 4 cm in size, originate from Rapid Creek and the Big Fish River in the Dawson mining district, Alaska (USA). Good quality specimens, measuring up to 1 cm, have also been discovered in Lavra da Ilha, Taquaral, Itinga, Minas Gerais, Brazil. In Spain, it appears in the form of crystals up to 1 cm found in cavities within montebrasite at the Tita mine in Golpejas, Salamanca.

References

References

  1. Warr, L.N.. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine.
  2. [http://rruff.geo.arizona.edu/doclib/hom/wardite.pdf Handbook of Mineralogy]
  3. [http://www.mindat.org/min-4242.html Mindat.org]
  4. [http://webmineral.com/data/Wardite.shtml Webmineral data]
  5. Gaines, R.V., W. Skinner, C.W., Foord, E.E., Mason, B. Rosenzweig, A.. (1997). "Dana's new mineralogy". John Wiley & Sons, Inc..
  6. "Wardite. Mindat".
  7. Robinson, G. W., Van Velthuizen, J, Ansell, H. G. y Sturman, B.D. "Mineralogy of the Rapid Creek and Big Fish River Area, Yukon Territory". The Mineralogical Record.
  8. Calvo, Miguel. (2015). "Minerales y Minas de España. Vol. VII. Fosfatos, Arseniatos y Vanadatos". Escuela Técnica Superior de Ingenieros de Minas de Madrid. Fundación Gómez Pardo.
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