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Identifying minerals (with slides from ‘duncanpatti’ and ‘ms. Wells’)

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Identifying minerals

(with slides from ‘duncanpatti’ and ‘ms. Wells’)

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A mineral:

1. Occurs naturally (not man-made) 2. is a solid 3. is a chemical compound arranged in

an orderly pattern (crystals) 4. is inorganic (not made from dead

plants or animals) 5. Is an element or a compound

What are minerals?

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Properties of Minerals:Which are the most important?

• Streak• Luster• Cleavage or Fracture• Density• Hardness

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Physical Properties of Minerals (can be used to identify the mineral)

Color• Can be misleading• Can vary with the type of impurities

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Physical Properties of Minerals (can be used to identify the mineral)

Luster• Surface

reflection • metallic = shiny

like metal• non-metallic =

dull, non-shiny surface

Pyrite has a metallic luster

Calcite has a non-metallic luster

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Metallic Luster

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Nonmetallic Luster

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Physical Properties of Minerals (can be used to identify the mineral)

Streak• The color of the powdered

form of the mineral• The color of the streak can be

different than the mineral• Minerals must be softer than

the streak plate

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Streak…can help identify quartz

http://www.childrensmuseum.org/geomysteries/cube/b3.html

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Breaking Properties:Cleavage or Fracture

• Cleavage – mineral breaks along a flat surface or into sheets

• Fracture – when a mineral breaks with lots of jagged edges

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Hardness = resistance to scratching Hardness does not concern

brittleness (brittle = breaks apart easily)

e.g. glass is brittle (breaks easily when dropped), but it is harder than copper, i.e. it can scratch copper.

copper cannot scratch glass

Mineral test #1: hardness

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Physical Properties of Minerals (can be used to identify the mineral)

Hardness• How easily a mineral scratches

materials• Mohs Hardness Scale

• Scale from 1 (softest) to 10 (hardest)• Test by seeing if the mineral can scratch

different objects (like human fingernail, copper, penny, glass, steel file)

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Talc(Mg3Si4O10(OH)2)

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Gypsum (CaSO4·2H2O)

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Calcite CaCO3

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Fluorite CaF2

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Apatite Ca5(PO4)3(F,Cl,OH)

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Feldspar KAlSi3O8 - NaAlSi3O8 - CaAl2Si2O8

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Quartz SiO2

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Topaz Al2SiO4(F,OH)2

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Corundum Al2O3

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(do you really need a picture?)

Diamond

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cleavage: tendency of a mineral to split easily or separate along flat surfaces

e.g. mica: 1 cleavagefeldspar: 2 cleavagescalcite: 3 cleavagesgalena: 3 cleavages

Mineral test #2: cleavage

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Physical Properties of Minerals (can be used to identify the mineral)

Cleavage & Fracture• The way the mineral breaks• Cleavage—minerals break

along smooth, flat surfaces and every fragment has the same general shape• Fracture—minerals that

break at random with rough or jagged edges

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Specific gravity: “how dense is the mineral compared to water?”

Nearly all minerals are denser than water.

Mineral test #3: specific gravity

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If a mineral is denser than water, its specific gravity is greater than 1.

If it is less dense than water, its specific gravity is less than 1.

If it is equally dense as water, its specific gravity equals 1.

specific gravity, cont’d

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Extra Special Properties

1. Fluorescence• Fluorescent color under ultraviolet (UV)

light2. Magnetic• Attract magnets

3. Acid reaction• Carbon dioxide gas bubbles off when

you drop acid on them• Carbonates!

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Fluorescence

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Magnetic

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Carbonate Acid Reaction