Editorial Feature

Fingerite - Occurrence, Properties, and Distribution

Fingerite is a triclinic-pinacoidal black mineral containing vanadium, oxygen and copper. It was first discovered in 1985 from Izalco volcano, El Salvador. The mineral was named after Larry W. Finger, American mineralogist, Carnegie Institution, Washington, D.C., USA.

Properties of Fingerite

The following are the key properties of Fingerite:

  • Cell Data
    • Space Group: P1
    • a = 8.1576(6)
    • b = 8.2691(5)
    • c = 8.0437(7)
    • α = 107.144(5)°
    • β = 91.389(7)°
    • γ = 106.441(5)°
    • Z = 1.
  • Crystal Data
    • Triclinic
    • Point Group: 1
    • As crystals, to 150 µm, may be subhedral or anhedral; equant or plate-like
    • Twinning: As contact and multiple twins, by rotation about [010]
    • X-ray Powder Pattern: 6.48 (100), 3.042 (80), 2.822 (70), 2.025 (70), 3.894 (60), 3.617 (60), 3.293 (60d).
  • Chemical Composition
    Elements Content 1 Content 2 Content 3
    CuO 59.3 59.53 61.59
    V2O5 39.65 39.67 38.41
    Total 98.95 99.20 100
  • Optical Properties
    • Optical Class: Biaxial.
  • Estimated Properties
    Electron density Bulk density (electron density) = 4.48 g/cm3
    note: Specific gravity of Fingerite = 4.78 g/cm3
    Photoelectric PEFingerite = 26.34 barns/electron
    U = PEFingerite x ρElectron density = 117.86 barns/cm3
    Fermion index Fermion index = 0.0006
    Boson index = 0.9993
    Radioactivity
    Fingerite is not radioactive.

How to Identify Fingerite

Fingerite is an opaque black mineral having a dark red brown streak and metallic luster.

Global Distribution

Fingerite is widely found in the Izalco volcano, El Salvador.

Occurrence of Fingerite and Useful Mineral Association

Fingerite occurs as a rare component of vanadium-bearing sublimates in fumaroles on a basaltic volcanic cone, formed between 100 and 200°C.

References

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