Editorial Feature

Apachite - Occurrence, Properties, and Distribution

Apachite is a copper silicate mineral first discovered from Christmas Mine, Gila, Arizona, USA in 1979. The mineral was named for the Apache Indians, whose reservation is near the locality.

Properties of Apachite

The following are the key properties of Apachite:

  • Cell Data
    • Space Group: n.d
    • a = 12.89
    • b = 6.055
    • c = 19.11
    • β = 90:42°
    • Z = [2]
  • Crystal Data
    • Monoclinic
    • Point Group: n.d
    • As minute, twisted or curved beaded spherules of radial fibers, composed of crystals; in seams, exhibiting a silky, fibrous structure on broken surfaces
    • X-ray Powder Pattern: 12.89 (100), 3.168 (70), 7.663 (50), 10.62 (40), 9.556 (40), 4.491 (40), 4.174 (40).
  • Chemical Composition
    Elements Content 1 Content 2
    CuO 43.6 47.26
    SiO2 40.8 39.66
    H2O 13.8 13.08
    CaO 1.8 -
    MgO 1.7 -
    FeO 0.3 -
    Total 102 100
  • Optical Properties
    • Optical Class: Biaxial (-)
    • Orientation: Y ≃ length
    • α = 1.610
    • β = 1.650
    • γ = 1.650
    • 2V(meas.) = Small.
  • Estimated Properties
    Electron density Bulk density (electron density) = 3.31 g/cm3
    note: Specific gravity of Apachite = 3.37 g/cm3
    Photoelectric PEApachite = 16.97 barns/electron
    U = PEApachite x ρ Electron density = 56.11 barns/cm3
    Fermion index Fermion index = 0.008
    Boson index = 0.99

    Radioactivity

    Apachite is not radioactive.

How to Identify Apachite

Apachite is a translucent blue-colored mineral with a light blue streak. The mineral exists as spherical, rounded aggregates or radial crystals. The average density of apachite is 2.8 g/cm3, and this mineral has a hardness of 2.

Global Distribution

Apachite is widely distributed in Christmas copper mine, Gila Co., Arizona, USA.

Occurrence of Apachite and Useful Mineral Association

Apachite occurs as a retrograde metamorphic or mesogene mineral formed at the expense of a prograde calc-silicate in tactites. It can also be observed in fractures or crackled zones cutting garnet-diopside rock, replacing both these silicates and calcite. The mineral is closely associated with tobermorite, calcite, apophyllite, xonotlite, clinohedrite, junitoite, stringhamite, gilalite and kinoite.

References

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