1. MINERALS

2. DEFINITION A mineral is: Naturally occurring substance Inorganic (not living) Solid Has a definite (specific) crystal structure Made of a specific chemical compound

3. CLASSIFICATION OF MINERALS How minerals are identified is called, classification. Using the following tests, the exact mineral can be determined

4. COLOR Color – this is NOT a good clue to the identity of a mineral because many minerals are found in several colors and many minerals have extra chemicals in them that give them an unexpected color. Weathering may also change the color of the mineral. Example: quartz comes in various colors: rose, milky, clear

5. LUSTER Luster - the way a mineral reflects light. Minerals can be described as metallic, pearly, glassy, silky, greasy, brilliant, or dull. Example: diamonds are brilliant. Talc has a greasy luster, quartz has a glassy luster, and gypsum has a pearly luster. Pyrite or fool's gold, as it is sometimes called, has a metallic luster.

6. STREAK Streak - the color of the streak made by rubbing a mineral across a hard, rough surface like a bathroom tile which is known as the streak test Example: is pyrite which is a brassy, yellow color. However, it makes a greenish, black streak when rubbed across a rough surface. You will need a field guide to rocks and minerals to tell you what color streak a mineral makes.

7. CLEAVAGE AND FRACTURE Cleavage & Fracture are when certain minerals break in a definite way. Cleavage = square or flat sides Fracture = irregular breaks Example: Galena cleaves into little cubes. Mica cleaves into thin sheets. Calcite cleaves into slanting bricks. Feldspar breaks into little steps. Quartz cleaves into irregular chunks.

8. HARDNESS Hardness is measured by seeing how easy it is to scratch a mineral which is known as the scratch test Example: talc, the softest mineral known, can be scratched with a fingernail. Diamond, the hardest mineral, can scratch all the other minerals but cannot be scratched by them. A German mineralogist, Friedrich Mohs, developed a standard scale of hardness in 1822. His scale is so easy to use that it is still in use today. mineralogist scale of hardness

9. MOHS HARDNESS SCALE Mineral ExampleDescription 1TalcFingernail scratches it easily. 2GypsumFingernail scratches it. 3CalciteCopper penny scratches it. 4FluoriteSteel knife scratches it easily. 5ApatiteSteel knife scratches it. 6FeldsparSteel knife does not scratch it easily, but scratches glass. 7QuartzHardest common mineral. It scratches steel and glass easily. 8TopazHarder than any common mineral. 9CorundumIt scratches Topaz. 10DiamondIt is the hardest of all minerals.

10. SPECIFIC GRAVITY/DENSITY Specific gravity of a mineral is its relative weight compared to the weight of an equal volume of water. It determines the density of the mineral. Example: Two minerals may be the same size, but their weight may be very different. Water has a specific gravity of 1. If a mineral has a specific gravity less than 3, it is considered a "light" mineral, between 3 and 5 - "average", and more than 5 - "heavy". Minerals with a metallic luster are usually "heavy".

11. CRYSTAL STRUCTURE Specific and regular crystal patterns

12. OTHER PROPERTIES Acid Test – whether it reacts to acid Magnetism – whether there is a push or pull against other metals

13. PROCESSES THAT RESULT IN THE FORMATION OF MINERALS The processes that result in the formation of minerals are The cooling and crystallization from magma/lava Bigger crystals form when it cools slowly Evaporation of liquid from a solution

14. MAJOR GROUPS OF MINERALS The two major groups of minerals is silicate and non-silicate minerals. Silicate minerals contain Silicate groupings. Silicate minerals are minerals that have a combination of silicon and oxygen. Non-silicate minerals do not contain silicate. Non-silicate minerals are minerals that do not have a combination of silicon and oxygen.

15. SULFIDES AND SULFATES Sulfate is a combination of oxygen and sulfur whereas sulfide is the negative ion of sulfur alone. Both are negative ions. Both sulfur and oxygen are "hungry" for electrons. When they make a chemical bond it is to gain a share of electrons to put them into a more stable electron mode (or configuration). The suffix '-ate' in chemistry indicates that there is oxygen present whereas '-ide' tells us that only the element alone is present in forming the ion.

16. USES OF MINERALS Gems – jewelry Metals – strength Ores – mined for a profit Smelt – the melting of minerals

17. MINING Open Pit Mining Shaft Mining Strip Mining

18. ENVIRONMENTAL IMPACT Waste materials Depletion of resources Damage to surface or cause sink holes in caves