 Natural  Solid  Inorganic  Definite chemical composition  Crystal structure due to internal arrangement of atoms.

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Presentation transcript:

 Natural  Solid  Inorganic  Definite chemical composition  Crystal structure due to internal arrangement of atoms

 Aluminum--packaging, transport, building  Beryllium--gemstones, fluorescent lights  Copper--electric cables, wires, switches  Feldspar--glass and ceramics  Iron--buildings, automobiles, magnets  Calcite--toothpaste, construction

 hardness  crystal shape (form)  luster  color  streak  cleavage/fracture  density (specific gravity)  special properties - -reaction to acid - -fluorescence -- salty taste -- magnetism

 Ability to scratch another mineral  Mohs scale from 1 (talc) to 10 (diamond)  Quartz (most common mineral and most dust particles) is 7

 External structure due to internal arrangement of the atoms  Six basic groups of shapes, with about three dozen variations

 Describes how light reflects off the surface  Main categories are “metallic” and “non- metallic”  Non-metallic includes “dull,” glassy,” waxy,” “pearly,” and othershttp:// rals.net/mineral/sulfide s/pyrite/pyrite2.htm

 results from ability to absorb some wavelengths and reflect others  some minerals have characteristics colors  others vary due to chemical differences or impurities (atoms mixed inside the main elements)

 Color of the powder when rubbed on a “streak plate” (unglazed porcelain)  May be same as hand-specimen or different  Some paint is based on powdered minerals (streaks).

 Some minerals split along flat surfaces when struck hard--this is called mineral cleavage  Other minerals break unevenly along rough or curved surfaces--this is called fracture  A few minerals have both cleavage and fracture

 All minerals have density (mass / volume), but some are very dense  Examples include galena, magnetite, and gold  Specific Gravity is the density of the mineral compared with density of water

Carbonates react with dilute HCl and other acids by fizzing or bubbling (releasing CO2 gas)

 Some minerals will glow when placed under short-wave or long-wave ultraviolet rays  Franklin and Ogdensburg NJ are famous for their fluorescent minerals

 DO NOT TASTE MOST MINERALS!  Halite is the exception--it will taste salty

 Many iron minerals will produce an invisible magnetic force field  “Lodestone” was used by Vikings more than 1,000 years ago as compasses