Physical observations from uncut gems

Simple tests are used to help identify a gem.
  1. Hardness: mohs hardness scale and other measurements. Although a somewhat destructive test, hardness values can be quite diagnostic.

  2. Cleavage: preferential breakage along some surfaces e.g., mica. The planes along which minerals break are planes where atomic bonds are weaker.

  3. Streak: color of powdered material when scraped across a ceramic tile.
  1. Crystal Morphology: The external shape of crystals, reflects the crystal symmetry, and thus the atomic arrangement.

    e.g., hexagonal prism vs. octahedra. This is based on internal atomic order and can not be determined from faceted crystals !

Observations from cut and uncut gems

Note that some of these measurements are only possible if the gem stone is removed from its setting!

  1. Color: generally unreliable! It MAY be a clue (note the luster).

  2. Specific Gravity
    • Specific gravity is measured by comparing the weight of the gem in air with its weight suspended in water

    • density = amount of mass per given volume: measured as grams per cubic centimeter.

    Specific gravity varies with chemical composition and crystal structure type.

    1. Refractive Index

      These measurements are relatively straight forward for stones in settings.

    2. Dispersion: the extent to which blue light is bent more than red light as it passes from air into a crystal (dispersion) can be measured and the value compared to tabulated values.

    3. Pleochroism: A mineral whose color changes with its orientation is said to be pleochroic or to exhibit pleochroism.

      Specific minerals exhibit specific pleochroic colors. Cabochons of Cordierite exhibit this phenomena very clearly.

    4. Other techniques (EPS 2 students are not required to be familiar with these): Spectroscopic techniques: X-ray images (e.g. of pearls) or X-ray Diffraction (used for the measurement of the atomic arrangement). Other techniques include Raman and Electron Microprobe. Spectroscopies revealing absorption details are especially important.

    Other optical properties:

    The behavior of light as it passes into a crystal depends upon the structure and chemistry of the mineral.

    An important test involves the use of two polarizing filters that are oriented nnormal to one another.

    Note that in the absence of a crystal between the two sheets of polaroid, light is completely absorbed at the second sheet of polaroid.

    The crystal is placed between the polaroid filters and the result is observed.

    • Optical behavior is subdivided into three types:

      • Isotropic: material always remains dark under cross polarized light

      • Anisotropic: light passes through the crystal as it is rotated under crossed polars.
      • If, as it is rotated about one specific axis (only), the crystal remains dark, then the gem is termed "uniaxial".
      • If two specific axes can be found where the crystal remains dark while rotated between two crossed polars, the crystal is termed "biaxial".
      • Gems are classified firstly on isotropic, uniaxial, or biaxial categories, and then into more specific crystal systems.

    Determination of optical properties allows a gem to be assigned into a group, each group is consistent with either one or a small subset of the possible crystal systems. This can often be used to distinguish between possible identifications. If you don't understand how this works, please look at these examples

    "What is a Crystal?

    "Diamonds and Diamond Simulants"

    To concepts section


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