1. Identifying Minerals
Each mineral has its own specific chemical and physical properties used to identify it.

2. Color The same mineral can come in a variety of colors
Ex. quartz
Impurities & other factors can change mineral appearance
Color is not the best way to identify minerals

3. Luster - Describes how a surface reflects light (shiny/dull)
Metallic- minerals containing metals are often shiny
Nonmetallic
Vitreous- glassy, brilliant
Silky-fibrous
Resinous-plastic
Waxy- greasy, oily
Pearly- creamy
Earthy- rough, dull

4. Streak Color of mineral in powder form
Observed by rubbing a mineral against a piece of unglazed porcelain called a streak plate
Streak doesn’t vary like color & is often different than a mineral’s color
More reliable than color

5. Cleavage and Fracture
Way a mineral breaks apart determined by arrangement of atoms
Cleavage- breaks along flat surfaces
Fracture- mineral breaks in an irregular way

6. Hardness Minerals resistance to being scratched
Ranks minerals from softest to hardest
Talc- softest known mineral
Diamond- hardest known mineral

7. Density D = m/V Mass in a given space/ mass per unit volume 
Density remains same regardless of sample size

8. Special Properties
Fluorescence- minerals glow under ultraviolet light, ex. fluorite & calcite
Magnetism- ex. Magnetite
Radioactive- ex. contain radium or uranium
Effervescence- mineral fizzes (releases carbon dioxide) when in contact with hydrochloric acid, ex. calcite