Editorial Feature

Acuminite – Occurrence, Properties, and Distribution

The term acuminite was coined from the Latin word acuminis, meaning sharp point, or spear head, to denote the characteristic shape of the crystals in the mineral. It is an aluminum complex salt.

Properties of Acuminite

The following are the key properties of acuminite:

  • Cell Data
    • Space group: C2/c or Cc
    • a = 13.223(1)
    • b = 5.175(1)
    • c = 14.251(1)
    • β = 111.61(2)°
    • Z = 8

  • Crystal Data
    • Monoclinic
    • Point group: 2/m or m
    • As acute di-pyramidal crystals, showing {110}, {111}, and rare {112}, similar to spearheads, to 1mm
    • Twinning: On {100}, as contact twins
    • X-ray powder pattern: 4.767 (10), 4.706 (10), 3.505 (10), 3.353 (10), 2.075 (9), 3.310 (8), 3.286 (8)

  • Chemical Composition
    Elements Content 1 Content 2
    Sr 37.04 38.84
    F 33.52 33.68
    Al 11.86 11.96
    H2O [7.80] 7.98
    OH [6.82] 7.54
    Ca 0.02 -
    Total [97.06] 100.00

  • Optical Properties
    • Transparent
    • Optical Class: Biaxial (+)
    • Orientation: X = b; Y^c = 15(1)°
    • Dispersion: r > v, strong
    • α = 1.4507(3)
    • β = 1.4528(3)
    • γ = 1.4624(3)- 1.4627(3)
    • 2V(meas.) = 46°-57°

  • Estimated Properties
    Electron density Bulk density (electron density) = 3.11 g/cm3
    note: Specific gravity of acuminite = 3.31 g/cm3.
    Photoelectric PEAcuminite = 44.23 barns/electron
    U = PEAcuminite x ρ electron density = 137.56 barns/cm3
    Fermion index Fermion index = 0.02
    Boson index = 0.98
    Radioactivity
    Acuminite is not radioactive

How to Identify Acuminite

Acuminite can be identified in the field by its colorless structure, with white streak, and vitreous luster.

The density of acuminite is 3.295 g/cm3, with a hardness of 3.5 – approximate to a copper penny.

Global Distribution

Acuminite is distributed chiefly in the Ivigtut cryolite deposit, south-western Greenland.

Occurrence of Acuminite and Useful Mineral Association

Acuminite occurs in a small cavity in a specimen from a strontium-rich portion of a cryolite deposit.

It is often associated with minerals such as pachnolite, fluorite, ralstonite, gearksutite, celestine, jarlite, and thomsenolite.

References

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