Mineral Formation. Methods of Formation Crystals may form from magma cooling Cools slow = large...

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Mineral Formation

Transcript of Mineral Formation. Methods of Formation Crystals may form from magma cooling Cools slow = large...

Page 1: Mineral Formation. Methods of Formation Crystals may form from magma cooling Cools slow = large crystals Cools quickly = small crystals Confined space.

Mineral Formation

Page 2: Mineral Formation. Methods of Formation Crystals may form from magma cooling Cools slow = large crystals Cools quickly = small crystals Confined space.

Methods of Formation

Crystals may form from magma cooling Cools slow = large crystals Cools quickly = small crystals Confined space = small crystals Open space = large crystals

Crystals may form out of solution. As liquid evaporates, mineral is left behind Ex/ “Bad Koolaide”, sea salt on skin

Page 3: Mineral Formation. Methods of Formation Crystals may form from magma cooling Cools slow = large crystals Cools quickly = small crystals Confined space.
Page 4: Mineral Formation. Methods of Formation Crystals may form from magma cooling Cools slow = large crystals Cools quickly = small crystals Confined space.

Silicates

Structure of all silicates is a Tetrahedron

1 Silicon & 4 Oxygen arranged in a pyramid structure

96% of minerals are known as silicates.

Oxygen nearly 50% of the Earth’s crust. Silicon makes up over 27%

Page 5: Mineral Formation. Methods of Formation Crystals may form from magma cooling Cools slow = large crystals Cools quickly = small crystals Confined space.

Carbonates & Oxides

Carbonates

Metal + carbonate CO3

Fizz in the presence of HCl acid

Ex/ marble, limestone, & calcite

Oxides

Metal + oxygen

Good sources of iron

Ex/ Magnetite & Hematite

Page 6: Mineral Formation. Methods of Formation Crystals may form from magma cooling Cools slow = large crystals Cools quickly = small crystals Confined space.

Other Mineral Groups

Sulfides = sulfur + another element (Pyrite)

Sulfates = sulfate (SO4) + another element

Halides = Cl or F (fluorine) bonded with a calcium, sodium or potassium

Native elements = made of one element only (Gold, Silver, Sulfur, etc.)

Page 7: Mineral Formation. Methods of Formation Crystals may form from magma cooling Cools slow = large crystals Cools quickly = small crystals Confined space.

Mineral Use Categories

Remember that minerals make up the entire crust Making up rocks On their own

Many are used for economic reasons

2 economic categories Ore minerals Gems

Page 8: Mineral Formation. Methods of Formation Crystals may form from magma cooling Cools slow = large crystals Cools quickly = small crystals Confined space.

Ore Minerals

Ore: mineral found with in deposits that can be profitably mined

This means that the money earned from the ore itself outweighs the cost of extracting it

Most ores are found as compoundsWhile many precious metals are native

Page 9: Mineral Formation. Methods of Formation Crystals may form from magma cooling Cools slow = large crystals Cools quickly = small crystals Confined space.

Ore Examples

Chalcopyrite: mined for Copper

Galena: mined for Lead

Sphalerite: mined for Zinc

Halite: mined for table salt

Gypsum: Sheet rock (dry wall) & plaster

Hematite: source of Iron

Bauxite: source of Aluminum

Page 10: Mineral Formation. Methods of Formation Crystals may form from magma cooling Cools slow = large crystals Cools quickly = small crystals Confined space.

Gems

Gems are valuable for their beauty rather than their industrial uses Precious Semi-precious

The rarer the gem, the more valuableEmeralds & Rubies are actually more valuable than

diamonds

Trace elements can make an ordinary mineral more prized Ex/ Amethyst: form of quartz; trace elements make it purple

Page 11: Mineral Formation. Methods of Formation Crystals may form from magma cooling Cools slow = large crystals Cools quickly = small crystals Confined space.

More on Gems

PreciousDiamonds

Emeralds

Rubies

Sapphires

Opals

Semi-preciousAmethystJasperAgateTiger EyeSometimes Turquoise Topaz Garnet