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Woodhouseite


FieldValue
nameWoodhouseite
categoryPhosphate minerals
boxwidth24
imagewoodhouseite 01.jpg
captionWoodhouseite from the type locality, the Champion Mine, Mono County, California, US. Specimen width is 2.8 cm
formulaCaAl3(SO4)(PO4)(OH)6
IMAsymbolWdh
molweight414.10 g/mol
strunz8.BL.05
dana43.04.01.08
systemTrigonal
classHexagonal scalenohedral ( 2/m)
symmetry*Rm* (no. 166)
colorWhite, flesh-pink or colorless
habitCrystals small, pseudocubic rhombohedral {1012}; tabular at times {0001}, with curved and striated faces.
cleavageExcellent on {0001}
mohs4.5
lusterVitreous, pearly on {0001}
refractive(AM22) nω = 1.636
nε = 1.647
opticalpropUniaxial (+), 2V = 0° to 20°
birefringenceδ = 0.011
streakWhite
gravity(measured): 3.012 (calculated): 3.00
solubilitySoluble in acids only after driving off the water in a closed tube.
diaphaneityTransparent to translucent
otherNot radioactive.
references

nε = 1.647 Woodhouseite belongs to the beudantite group AB3(XO4)(SO4)(OH)6 where A = Ba, Ca, Pb or Sr, B = Al or Fe and X = S, As or P. Minerals in this group are isostructural with each other and also with minerals in the crandallite and alunite groups. They crystallise in the rhombohedral system with space group Rm and crystals are usually either tabular {0001} or pseudo-cubic to pseudo-cuboctahedral. Woodhouseite was named after Professor Charles Douglas Woodhouse (1888–1975), an American mineralogist and mineral collector from the University of California, Santa Barbara, US, and one-time General Manager of Champion Sillimanite, Inc.

Environment

Woodhouseite is a secondary mineral found where wall rock alteration occurred in hydrothermal and disseminated ore deposits; rare in cave deposits, formed from guano. At the type locality it occurs in vugs in quartz veins in an andalusite, Al2OSiO4, deposit. This is in pre-Cambrian meta-quartzite that has been intruded by late Jurassic granitic rocks. Woodhouseite is found only near masses of lazulite, MgAl2(PO4)2(OH)2. Associated Minerals at the type locality include topaz, Al2SiO4F2, quartz, SiO2, augelite, Al2PO4(OH)3, lazulite, MgAl2(PO4)2(OH)2, tourmaline, baryte, BaSO4, muscovite, KAl2(Si3Al)O10(OH)2, and pyrophyllite, Al2Si4O10(OH)2, all of which formed before the woodhouseite, which is a late-forming mineral.

Localities

The type locality is the Champion Mine (White Mountain Mine), White Mountain, Laws, White Mountains, Mono County, California, US. This is a former sillimanite mine located near Laws; mineralisation is a metamorphic sillimanite deposit hosted in quartzite.

Structure

Space Group: R 2/m

Unit Cell Parameters: a = 6.993 Å, c = 16.386 Å, Z: 3

References

References

  1. Warr, L.N.. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine.
  2. "Woodhouseite Mineral Data".
  3. http://www.mindat.org/min-4311.html Mindat.org
  4. http://rruff.geo.arizona.edu/doclib/hom/woodhuseite.pdf Handbook of Mineralogy
  5. "University of California: In Memoriam, May 1977".
  6. Lemmon, Dwight M (1937) American Mineralogist 22:939-948
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