Although we have discussed x-ray identification of minerals and later in the course will discuss techniques that can be used to identify minerals with the optical microscope, it is still necessary to develop techniques that can be used in the laboratory and field where instrumentation like x-ray diffractometers or microscopes cannot be easily used.  Minerals have distinguishing physical properties that in most cases can be used to determine the identity of the mineral.  In this course, you will develop a systematic approach to using the physical properties of minerals as identifying tools.  If you follow this approach you should be able to identify most of the common minerals, or at the least be able to narrow the possibilities to only a few.  We will first discuss each of the physical properties that can be used, then develop a methodical approach to the identification of minerals using these physical properties.  Among the properties we will discuss are: crystal habit, cleavage, hardness, density, luster, streak, color, tenacity, magnetism, and taste.

Some common crystal habits are as follows (discussed previously):

Individual Crystals

• Cubic - cube shapes
  
  
• Octahedral - shaped like octahedrons, as described above.
  
  
• Tabular -  rectangular shapes.
  
  
• Equant - a term used to describe minerals that have all of their boundaries of approximately equal length.
  
  
• Acicular -  long, slender crystals.
  
  
• Prismatic -  abundance of prism faces.
  
  
• Bladed -  like a wedge or knife blade.

Groups of Distinct Crystals

• Dendritic - tree-like growths.
  
  
• Reticulated - lattice-like groups of slender crystals.
  
  
• Radiated - radiating groups of crystals.
  
  
• Fibrous -  elongated clusters of fibers.
  
  
• Botryoidal - smooth bulbous or globular shapes.
  
  
• Globular - radiating individual crystals that form spherical groups.
  
  
• Drusy - small crystals that cover a surface.
  
  
• Stellated - radiating individuals that form a star-like shape.

Some minerals characteristically show one or more of these habits, so habit can sometimes be a powerful diagnostic tool.

Cleavage can also be described by general forms names, for example if the mineral breaks into rectangular shaped pieces it is said to have cubic cleavage, if it breaks into prismatic shapes, it is said to have prismatic cleavage, or if it breaks along basal pinacoids it is said to have pinacoidal cleavage.  For examples, see figure 2.12 on page 29 of your text.

Parting

Parting is also a plane of weakness in the crystal structure, but it is along planes that are weakened by some applied force.  It therefore may not be apparent in all specimens of the same mineral, but may appear if the mineral has been subjected to the right stress conditions.

Fracture

If the mineral contains no planes of weakness, it will break along random directions called fracture.  Several different kinds of fracture patterns are observed.

• Conchoidal fracture - breaks along smooth curved surfaces.
  
• Fibrous and splintery -  similar to the way wood breaks.
  
• Hackly - jagged fractures with sharp edges.
  
• Uneven or Irregular - rough irregular surfaces.

Several precautions are necessary for performing the hardness test. 

• If you attempt to scratch a soft mineral on the surface of a harder mineral some of the softer substance may leave a mark of fine powder on the harder mineral.  This should not be mistaken for a scratch on the harder mineral.  A powder will easily rub off, but a scratch will occur as a permanent indentation on the scratched mineral. 
  
  

• Some minerals have surfaces that are altered to a different substance that may be softer than the original mineral.  A scratch in this softer alteration product will not reflect the true hardness of the mineral.  Always use a fresh surface to perform the hardness test.
  
  

• Sometimes the habit of the mineral will make a difference.  For example aggregates of minerals may break apart leaving the impression that the mineral is soft. Or, minerals that show fibrous or splintery habit may break easily into fibers or splinters.  It is therefore wise to always perform the hardness test in reverse.  If one mineral appears to scratch another mineral, make sure that the other mineral does not scratch the apparently harder mineral before you declare which of the minerals is harder.
  
  

• In some minerals hardness is very dependant on direction, since hardness is a vectorial property.  When there is significant difference in hardness in different directions, it can be a very diagnostic property of the mineral.  It is thus wise to perform the hardness test by attempting to scratch the mineral in different directions.  Two minerals of note have differences in hardness depending on direction:
  
  

  • Kyanite has a hardness of 5 parallel to the length of the crystal, and a hardness of 7 when scratched along a direction perpendicular to the length.
    
    

  • Calcite has a hardness of 3 for all surfaces except the {0001} plane.  On {0001} it has a hardness of 2.

Tenacity is the resistance of a mineral to breaking, crushing, or bending.  Tenacity can be described by the following terms.

• Brittle - Breaks or powders easily.
  
  

• Malleable - can be hammered into thin sheets.
  
  

• Sectile - can be cut into thin shavings with a knife.
  
  

• Ductile - bends easily and does not return to its original shape.
  
  

• Flexible - bends somewhat and does not return to its original shape.
  
  

• Elastic - bends but does return to its original shape.

Density refers to the mass per unit volume.  Specific Gravity is the relative density, (weight of substance divided by the weight of an equal volume of water).  In cgs units density is grams per cm³, and since water has a density of 1 g/cm³, specific gravity would have the same numerical value has density, but no units (units would cancel).   Specific gravity is often a very diagnostic property for those minerals that have high specific gravities.  In general, if a mineral has higher atomic number cations it has a higher specific gravity.  For example, in the carbonate minerals the following is observed:

For comparison, examine the following table:

Color

Color is sometimes an extremely diagnostic property of a mineral, for example olivine and epidote are almost always green in color.  But, for some minerals it is not at all diagnostic because minerals can take on a variety of colors.  For example quartz can be clear, white, black, pink, blue, or purple.     Read in your textbook, pp. 234-240, about what causes minerals to have color. 

Streak

Streak is the color produced by a fine powder of the mineral when scratched on a streak plate.  Often it is different than the color of the mineral in non- powdered form

Luster

Luster refers to the general appearance of a mineral surface to reflected light.  Two general types of luster are designated as follows:

1. Metallic - looks shiny like a metal.  Usually opaque and gives black or dark colored streak.
   

2. Non-metallic - Non metallic lusters are referred to as
   
   

   1.  vitreous - looks glassy - examples: clear quartz, tourmaline
      
      

   2. resinous - looks resinous - examples: sphalerite, sulfur.
      

3. pearly - iridescent pearl-like - example: apophyllite.
   
   

4. greasy - appears to be covered with a thin layer of oil - example:  nepheline.
   
   

5. silky - looks fibrous. - examples - some gypsum, serpentine, malachite.
   
   

6. adamantine - brilliant luster like diamond.

Play of Colors

Interference of light reflected from the surface or from within a mineral may cause the color of the mineral to change as the angle of incident light changes.  This sometimes gives the mineral an iridescent quality.  Minerals that show this include: bornite (Cu₅FeS₄) , hematite (Fe₂O₃), sphalerite (ZnS), and some specimens of labradorite (plagioclase).

Fluorescence and Phosphorescence

Minerals that light up when exposed to ultraviolet light, x-rays, or cathode rays are called fluorescent.  If the emission of light continues after the light is cut off, they are said to be phosphorescent.  

Some specimens of the same mineral show fluorescence while other don't. For example some crystals of  fluorite (CaF₂) show fluorescence and others do not.  Other minerals show fluorescence frequently, but not always.  These include - scheelite (CaWO₄), willemite (Zn₂SiO₄), calcite (CaCO₃), scapolite (3NaAlSi₃O8^.(NaCl - CaCO₃), and diamond (C).

Magnetism

Magnetic minerals result from properties that are specific to a number of elements. Minerals that do not have these elements, and thus have no magnetism are called diamagnetic.  Examples of diamagnetic minerals are quartz, plagioclase, calcite, and apatite.  Elements like Ti, Cr, V, Mn, Fe, Co, Ni, and Cu can sometimes result in magnetism.  Minerals that contain these elements may be weakly magnetic and can be separated from each other by their various degrees of magnetic susceptibility. These are called paramagnetic minerals.  Paramagnetic minerals only show magnetic properties when subjected to an external magnetic field.  When the magnetic field is removed, the minerals have no magnetism.

Ferromagnetic minerals have permanent magnetism if the temperature is below the Curie Temperature.  These materials will become magnetized when placed in a magnetic field, and will remain magnetic after the external field is removed.  Examples of such minerals are magnetite, hematite-ilmenite solid solutions (Fe₂O₃ - FeTiO₃), and pyrrhotite (Fe_1-xS).

Other Properties 

Other properties that may be diagnostic include  chatoyancy, asterism, piezoelectricity,  and taste. Familiarize yourself with the meanings of these terms.  And watch for these properties as you examine minerals.

Tables for Identification of Minerals

Beginning on page 604 of your textbook is a table of determinative tables which should aid you in using physical properties of minerals to identify them.  Note that the tables are broken first into two different groups based on Luster.  Within each group, the minerals are then further divided on the basis of streak, hardness, and cleavage.  In the remarks column are listed other useful diagnostic property for each mineral.  Again, I encourage you to develop a systematic approach to identifying minerals.

Luster - Metallic or Submetallic

1. Hardness < 2½
   
2. Hardness > 2½. <5½.
   
3. Hardness > 5½.

Luster - Nonmetallic

1. Streak Colored
   
2. Streak Colorless
   
   1. Hardness < 2½
      
   2. Hardness >2½, < 3
      
      1. Cleavage prominent.
         
      2. Cleavage not prominent.
         
   3. Hardness >3, <5½.
      
      1. Cleavage prominent.
         
      2. Cleavage not prominent.
         
   4. Hardness >5½, <7
      
      1. Cleavage prominent.
         
      2. Cleavage not prominent.
         
   5. Hardness >7
      
      1. Cleavage prominent
         
      2. Cleavage not prominent.