Allactite

(repeating unit)Mn7(AsO4)2(OH)8IMA symbolAla[1]Strunz classification8.BE.30Dana classification41.2.1.1Crystal systemMonoclinicCrystal classPrismatic (2/m)
(same H-M symbol)Space groupP21/aUnit cella = 11.03, b = 12.12
c = 5.51 [Å], β = 114°, Z = 2IdentificationColorBrown, dark to light purplish red, brownish red, colorless to whiteCrystal habitElongated prisms, bladed, tabular, rosette-like aggregatesCleavageDistinct, {001}FractureUnevenTenacityBrittleMohs scale hardness4.5LusterVitreous, slightly greasy on fracture surfacesStreakGray to faint brownSpecific gravity3.83 (meas.), 3.94 (calc.)Optical propertiesBiaxial (−)Refractive indexnα = 1.755–1.761
nβ = 1.772–1.786
nγ = 1.774–1.787PleochroismX = blood-red; Y = pale yellow; Z = sea-green2V angle~0°References[2][3][4]

Allactite is a rare arsenate mineral of metamorphosed manganese zinc ore deposits. It is found in Sweden and New Jersey, US. Its name originated from Greek αλλάκτειν (allaktein) meaning "to change", referring to the strong pleochroism of the mineral.[3]

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. ^ Allactite. Mindat
  3. ^ a b Allactite. Handbook of Mineralogy
  4. ^ Moore P. (1968). "Crystal chemistry of the basic manganese arsenate minerals: II. The crystal structure of allactite" (PDF). American Mineralogist. 53: 733–741.

Bibliography

  • Palache, P.; Berman H.; Frondel, C. (1960). "Dana's System of Mineralogy, Volume II: Halides, Nitrates, Borates, Carbonates, Sulfates, Phosphates, Arsenates, Tungstates, Molybdates, Etc. (Seventh Edition)" John Wiley and Sons, Inc., New York, pp. 785-787.
  • v
  • t
  • e