Graphite specimen for virtual mineral identification, photograph by Sean  C. Murphy, 2020.

There are thousands of different minerals, and each of those minerals has a unique set of physical properties, These are not only useful for identifying minerals, but also for determining potential industrial uses of the minerals. A few are listed below.

Crystal Form

  • Mineral shape, if the mineral is allowed to grow unrestricted.

  • Controlled by crystalline structure.

  • Well developed crystals are relatively rare, so this may not help with mineral identification.

  • Making it more complicated, many minerals have more than one crystal form.


Color

  • Color is the most obvious physical property and most deceptive.

  • It is common for minerals to have more than one color.

  • Color is controlled by chemical composition - sometimes trace chemicals can impart color.


Streak

  • All minerals have a streak color, it’s controlled by chemical composition.

  • The color of a mineral that is powdered.

  • Streak color of a mineral shows less variation than its color.

  • Most minerals have only one streak color.


Luster

  • Appearance and intensity of light reflected from the mineral surface.

  • Two main groups:

    • Metallic - looks like metal.

    • Non-metallic - doesn't look like metal.

  • Non-metallic descriptions include silky, pearly, earthy, adamantine, vitreous, resinous.

  • Controlled by chemical composition and crystal structure.

  • Generally, not very useful for identification.


Fracture

  • Definition: manner in which a mineral breaks, but not along a plane of weakness.

  • All minerals have fracture. It’s controlled by crystal structures and chemical bonding.

  • Similar to cleavage

  • Conchoidal fracture - break looks like broken glass.

  • Irregular fracture (self-descriptive)


Cleavage

  • Tendency of a mineral to break along a plane of weakness within crystalline structure.

  • Controlled by crystalline structure and chemical bonding.

  • 0, 1, 2, 3, 4, and 6 cleavage planes can exist.

  • Most difficult physical property for students to understand and identify.

Hardness

  • Ability of a mineral to resist abrasion.

  • Controlled by the crystalline structure and the type of chemical bonds.

  • stronger bonds = harder mineral

  • Measured using Mohs Scale of Hardness

Busch, R. M., Ed., 2000, Laboratory manual in physical geology: Prentice Hall.Used according to Creative Commons license:


Other physical properties, that can definitively identify some unique minerals:


Magnetism

  • Some minerals contain enough iron (other metals) to generate an electromagnetic force.

  • Running a small magnet across a mineral, one can feel if there is an attraction.

Taste

  • Strange as it sounds, some minerals can be identified by taste (e.g., halite, or salt).

  • Do not lick introductory lab specimens (could be poisonous, and who knows who, before you?)

Hydrochloric acid

  • Dilute HCl reacts with Calcite (CaCO3) bubbling off CO2, distinguishing from Dolomite

  • Acids are dangerous, and can damage some valuable minerals. Be careful.

Radioactivity

  • Not a common physical property

  • Useful in some sedimentary rocks to identify presence of radioactive minerals.

  • Collectors use Geiger counter for detecting unusual minerals in pegmatites.

Specific Gravity

  • Ratio of the mass of a given volume of mineral to the mass of an equal volume of water

  • Not measured directly in introductory, but the “heft” of certain minerals is distinctive

  • Galena (Pb) is a good example

Fluorescence

  • Some minerals luminesce (“glow”) in presence of ultraviolet light from excited electrons

  • Short-wave ultraviolet lamps (100-280nm) can cause blindness and should not be viewed directly