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ROCKS & MINERALS

TOPIC 11

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  • Minerals are the ingredients of rocks.

Or

  • Rocks are made up of minerals.

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Minerals

  • Defn: naturally occurring, inorganic elements or compounds with specific physical and chemical properties.

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Mineral Properties

  • Used to identify minerals

  1. Color
  2. Least useful property in identifying minerals.
  3. Why?

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All of these are varieties of quartz!

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  1. Streak
  2. The color of a minerals powder.
  3. “streak test”

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  1. Luster
  2. How the minerals surface reflects light.
  3. Metallic vs. non- metallic.

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  1. Hardness
  2. The ability of a mineral to resist being scratched.
  3. “Scratch test”

  • If mineral A can scratch mineral B, what does that tell us about the relative hardness of each mineral?

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Moh’s Hardness Scale

Soft

Hard

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5. Fracture/ Cleavage

Fracture

  • Mineral breaks unevenly or irregularly

Cleavage

  • The tendency of a Mineral to break evenly along its weakest plane.

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  1. Crystal Form
  2. Some minerals tend to form crystals that aid in the identification of the mineral.

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  1. Specific Gravity
  2. The ratio of the density of the mineral to the density of water (1 g/cm3)

  • If a mineral has a specific gravity of 5 that means it is 5 times as dense as water.

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  1. Others
  2. Acid test – Calcite
  3. Magnetic – Magnetite
  4. Taste - Halite

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  • A minerals properties are due to the internal arrangement of its atoms.

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Silicate Minerals

  • Minerals that contain a combination of silicon and oxygen.

Silicon-oxygen tetrahedron

The basic structural unit of silicate minerals

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Rocks

Monomineralic

  • 1 Mineral

Polymineralic

  • More than 1 Mineral
  • Rocks are classified by how they are formed!!!

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Sedimentary Rocks:

  1. Clastics
  2. Rocks that form when sediments (sand, silt etc.) are lithified.

Processes

  • Compacting and cementing
  • Vary due to grain size! (see ref tables p. 7)

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  1. Non-Clastics
    1. Organics (bioclastics)
    2. Form from living things.

Examples: Coal, limestone

    • Chemical (crystaline)
    • Formed from the evaporation or precipitation of sea water.

Examples: Halite, gypsum

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Igneous:�- Form when liquid rock cools and solidifies

Intrusive

  • Cools below the earths surface (slowwwwly!)

  • Magma
  • “Plutonic”

Extrusive

  • Cools at the Earths surface (quickly!)

  • Lava
  • “Volcanic”

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  • The longer the rock takes to cool, the larger the crystals!

  • Cools slow …..Large crystals
  • Cools fast …….small crystals
  • Cools immediately……NO Crystals (glass)

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Vesicular- gas pockets

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Metamorphic:

  • Rocks that are changed due to extreme heat and/or pressure.
  • DO NOT MELT!!! (they recrystalize)

Metamorphic rocks become…

    • Harder
    • More dense
    • Banded or foliated
    • Distorted

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Banding

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Foliated

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Regional Metamorphism

  • Occurs when large areas of rock are changed.
  • Usually deep below the surface where crustal plates collide.

  • The Adirondacks!

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Contact Metamorphism

  • Occurs when liquid rock comes into contact with other rocks.

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Bedrock Of New York State

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Identifying Characteristics of Rocks

Igneous

  • Intergrown crystals
  • Glassy texture

Sedimentary

  • Cemented fragments (sediments)
  • Fossils
  • Organic material

Metamorphic

  • Banding
  • Foliated

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The Rock Cycle

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BONUS:

  • CLASSIFY this rock as igneous, sedimentary or metamorphic and EXPLAIN why you classified it that way.

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BONUS:

Name the mineral that has the following properties:

  • Non-metallic
  • Can scratch fluorite but cannot scratch quartz
  • Exhibits cleavage
  • Contains the elements sodium & hydrogen