Editorial Feature

Burgessite – Occurrence, Properties, and Distribution

Burgessite was named after David Burgess (1951-) of Newington in Connecticut, USA, who was a prolific mineral species collector.

Properties of Burgessite

The following are the key properties of burgessite :

  • Cell Data
    • Space group: P21/n
    • a = 4.7058(12)
    • c = 9.299(3)
    • c = 12.738(4)
    • β = 98.933(8)°
    • Z = 2

  • Crystal Data
    • Monoclinic
    • Point group: 2/m
    • Crystals, prismatic, to 0.1mm, forms {011} and {hol} observed
    • Typically as rosettes, to 0.8mm
    • X-ray powder pattern: 7.446 (100), 6.267 (44), 2.998 (31), 3.725 (29), 3.260 (25), 2.596 (23), 2.970 (21)

  • Chemical Composition
    Elements Content 1
    As2O5 47.91
    CoO 27.31
    H2O 22.65
    NiO 3.52
    CaO 0.18
    SO3 0.13
    ZnO 0.04
    P2O5 0.03
    Total 101.77

  • Optical Properties
    • Optical Class: Biaxial (+)
    • α = 1.596(2) ; β = 1.604(2); γ = 1.628(2)
    • 2V(meas.) = 70(2)°
    • 2V(calc.) = 61°
    • Orientation: X = b; Y ∧ c = 29° (in β obtuse); Z ∧ a = 20° (in β acute)

  • Estimated Properties
    Electron density Bulk density (electron density) = 2.85 g/cm3
    note: Specific gravity of burgessite = 2.94 g/cm3
    Photoelectric PEBurgessite = 28.90 barns/electron
    U=PEBurgessite x ρ electron density = 82.33 barns/cm3
    Fermion index Fermion index = 0.0005237727
    Boson index = 0.9994762273
    Radioactivity
    Burgessite is not radioactive

How to Identify Burgessite

Burgessite can be identified in the field by its purplish-pink color. Its transparent form has {010} good and {001} fair cleavage. This mineral has an adamantine luster, with pale pink streak. Its fracture is brittle and irregular.

The density of burgessite is 2.93 g/cm3, with a hardness of 3 – approximate to calcite.

Global Distribution

Burgessite is distributed mainly in Canada at the Keeley mine, South Lorraine Township, Timiskaming District, Ontario.

Occurrence of Burgessite and Useful Mineral Association

Burgessite typically occurs in a secondary mineral, along the fractures in the weathering zone of a polymetallic sulfarsenate deposit.

It is often associated with minerals such as skutterudite, bismuth, arsenolite, bismuthoferrite, erythrite, and cobaltite.

References

Tell Us What You Think

Do you have a review, update or anything you would like to add to this article?

Leave your feedback
Your comment type
Submit

While we only use edited and approved content for Azthena answers, it may on occasions provide incorrect responses. Please confirm any data provided with the related suppliers or authors. We do not provide medical advice, if you search for medical information you must always consult a medical professional before acting on any information provided.

Your questions, but not your email details will be shared with OpenAI and retained for 30 days in accordance with their privacy principles.

Please do not ask questions that use sensitive or confidential information.

Read the full Terms & Conditions.