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eld Trip #1: Hocking Hills State Saturday, October 2nd

Field Trip #1: Hocking Hills State Park Saturday, October 2nd

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Page 1: Field Trip #1: Hocking Hills State Park Saturday, October 2nd

Field Trip #1: Hocking Hills State ParkSaturday, October 2nd

Page 2: Field Trip #1: Hocking Hills State Park Saturday, October 2nd

MINERALS: The Building Blocks of Rocks

Page 3: Field Trip #1: Hocking Hills State Park Saturday, October 2nd

Definition of a Mineral

• A Mineral is a naturally occurring, inorganic, solid, crystalline substance, with definite physical and chemical properties.

• Inorganic – not composed of Carbon – Hydrogen molecules (usually part of living tissue)

• Crystalline – atoms have a structured arrangement.

Page 4: Field Trip #1: Hocking Hills State Park Saturday, October 2nd

CRYSTAL SHAPES

Page 5: Field Trip #1: Hocking Hills State Park Saturday, October 2nd

How Do Crystals Form?Remember Atomic Structure

Page 6: Field Trip #1: Hocking Hills State Park Saturday, October 2nd

ATOMS DO NOT WANT TO BE NEUTRAL THEY WANT TO BE STABLE

Stable Means Having Their Outer Shell Of Electrons Full To Capacity

This Can Happen By Losing Or Gaining Electrons to Other Atoms

This Process causes Atoms to Join Together: A Process Called Bonding

Page 7: Field Trip #1: Hocking Hills State Park Saturday, October 2nd

1) IONIC BONDING

Page 8: Field Trip #1: Hocking Hills State Park Saturday, October 2nd

2) COVALENT BONDING

Page 9: Field Trip #1: Hocking Hills State Park Saturday, October 2nd

OTHER BONDS3) Metallic – Electrons act as a mobile cloud that moves from atom to atom. Accounts for

excellent electrical conductivity of metals Example: Copper

4) van der Waals – Very weak Bond due to slight polarity of charge on atoms

Page 10: Field Trip #1: Hocking Hills State Park Saturday, October 2nd

MINERAL PROPERTIES: HARDNESS

Page 11: Field Trip #1: Hocking Hills State Park Saturday, October 2nd

MINERAL PROPERTIES: CLEAVAGEBreakage along planes of crystal weakness

Page 12: Field Trip #1: Hocking Hills State Park Saturday, October 2nd

MINERAL PROPERTIES: Other PropertiesColorStreak – color of powdered mineral Luster – the way light reflects of a mineralSpecific Gravity – Weight of Mineral

Weight of same volume of water

Fracture – breakage through crystalReactivity – Reacts with Acid?

Page 13: Field Trip #1: Hocking Hills State Park Saturday, October 2nd

MAJOR MINERAL GROUPSWhat are the most common minerals in the Crust?

1) What are the most common elements?

Page 14: Field Trip #1: Hocking Hills State Park Saturday, October 2nd
Page 15: Field Trip #1: Hocking Hills State Park Saturday, October 2nd

1) SILICATES – Made From Silicon + Oxygen> 91% of all crustal minerals

The Silicon – Oxygen Tetrahedron

Page 16: Field Trip #1: Hocking Hills State Park Saturday, October 2nd

The Silicon – Oxygen Tetrahedron can bond together in many different ways producing many different minerals

Page 17: Field Trip #1: Hocking Hills State Park Saturday, October 2nd

Other Important Mineral Groups

2) Carbonates – based on Carbonate ion (CO3) Calcite - Ca CO3, Dolomite - CaMg (CO3)2

Main component of the rocks limestone & dolostone.

3) Oxides – usually metals + oxygen Hematite - Fe2O3 (Iron Oxide or Rust), Corundum - Al2O3 (Aluminum Oxide or Ruby). Excellent source of ore metals

Page 18: Field Trip #1: Hocking Hills State Park Saturday, October 2nd

Other Important Mineral Groups

4) Sulfides – based on sulfide ion (S2-) Pyrite - FeS2 (“Fool’s Gold”) Excellent source of ore metals

5) Sulfates – based on sulfate ion (SO4)-

Gypsum - CaSO4 (Drywall) Used in the construction industry

Page 19: Field Trip #1: Hocking Hills State Park Saturday, October 2nd

So, why study minerals?1) Building Blocks of Rocks – what the Earth is made of.2) Important Economically – Industry & Agriculture.3) Can be incredibly beautiful!!