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Mineral Identification
Jul 7, 2024
Mineral Identification
Mineral Color
Color is not a reliable characteristic for identifying minerals.
Example: Quartz can come in many colors (white, blue, green).
Different minerals can share the same color.
Hardness
Measured using a piece of glass (hardness 5.5 on the Mohs scale).
Scratch test method:
Place glass on a table.
Try scratching the glass with a mineral sample.
If it scratches, the mineral's hardness is greater than 5.5.
If it doesn't, the mineral's hardness is less than 5.5.
Luster
Describes how light reflects off the surface of a mineral.
Two types for class: metallic and non-metallic.
Metallic:
Minerals that look like metal (e.g., Galena, Pyrite).
Non-metallic:
Minerals that do not look like metal (e.g., Olivine, Gypsum).
Breakage: Cleavage vs. Fracture
Fracture:
Random breakage with irregular shapes.
Examples: Olivine, Hematite, Quartz, Pyrite.
Cleavage:
Predictable breaking with flat surfaces.
Examples: Calcite (flat surfaces, predictable), Galena (90° angles), Halite, Biotite Mica (sheets).
Streak
The color of a mineral in powdered form.
Use streak plates (black and white ceramic tiles).
Procedure:
Rub the mineral on the streak plate to create powder.
Observe the color of the streak.
Examples:
Hematite: Reddish-brown streak.
Pyrite: Grayish-black streak.
Calcite: No streak or very faint white.
Other Properties
Taste:
Halite tastes salty (do not lick samples).
Magnetism:
Magnetite is magnetic.
Double Refraction:
Calcite doubles the image viewed through it.
Reaction with Acid:
Calcite fizzes when in contact with hydrochloric acid.
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