MINERAL PROPERTIES & Identification
MINERAL PROPERTIES & Identification
Over 4,000 minerals have been identified. Yet no
two are exactly alike.
HOW TO IDENTIFY MINERALS
Using: (physical properties)
Color – Can be used for identifying only a
few minerals.
Example: Mineral sulfur is always yellow.
Luster – Is the way light reflects from its
surface (“Shine”).
Two Types of Luster
1. Metallic – shiny, like metal
2. Nonmetallic – dull, earthy
Streak – Is the color of the powder left when a
mineral is rubbed against a hard rough surface.
Example: Mineral hematite makes red streak
Hardness – Is a mineral’s resistance to being
scratched.
[pic]
Moh's Hardness Scale – minerals 1-10 of increasing resistance to be scratched
1 softest – 10 hardest
[pic]
[pic]
Acid – carbonate
Hardness test: penny 3.5, nail 5.5, glass 6.5
Streak plate – color of powder
Magnet – test for iron and other magnetic minerals
Mineral Identification (cont.)
Density (Specific Gravity) – is the comparison of the density of a mineral to the density of water.
Water = 1 gm/cm³
Most minerals = 2.5-3.5 gm/cm³
Gold = 18 gm/cm³ silver, gold, galena (lead ore)
have high specific gravity
Cleavage or Fracture –
Is the way a mineral breaks or splits apart. Most minerals tend to break along smooth surfaces, if so the mineral has cleavage. If it shatters with jagged edges it is called fracture.
Diamond and gem cutters use cleavage planes to cut the faces in gems
Special properties
Carbonates give of gases when a weak acid is placed on them.
Example – calcite CaCO3
Acid Test – this is used for carbonate minerals.
Magnetic test – magnet sticks to the mineral
Magnetite (iron ore) “load stone”
Salty taste – cubic crystals of Halite (rock salt)
(do not ever taste minerals in lab)
geologist do this as a field test
Radioactive – give off charged particles (radiation)
Example: Uranium
Test with an instrument called a Geiger counter
Florescence – mineral glows under a U.V. light
(ultraviolet)
example: mineral fluorite and many others
Double refraction image – multiple images when viewed through clear crystal
Example: calcite
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