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© 2012 Pearson Education, Inc. Earth Science, 13e Tarbuck & Lutgens

Lecture Ch02

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Page 1: Lecture Ch02

© 2012 Pearson Education, Inc.

Earth Science, 13e

Tarbuck & Lutgens

Page 2: Lecture Ch02

© 2012 Pearson Education, Inc.

Matter and MineralsEarth Science, 13e

Chapter 2

Stanley C. Hatfield

Southwestern Illinois College

Page 3: Lecture Ch02

© 2012 Pearson Education, Inc.

Minerals: the building blocks of rocks

Definition of a mineral • Natural• Inorganic• Solid• Possess an orderly internal structure of

atoms • Have a definite chemical composition

Rock – any naturally occurring solid mass of mineral or mineral-like matter

Page 4: Lecture Ch02

© 2012 Pearson Education, Inc.

Composition and structure of minerals

Elements • Basic building blocks of minerals • Over 100 are known

Atoms• Smallest particles of matter • Have all the characteristics of an element

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Periodic table of the elements

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How atoms are constructed

Nucleus – central part of an atom that contains • Protons – positive electrical charges • Neutrons – neutral electrical charges

Energy levels, or shells • Surround nucleus • Contain electrons – negative electrical

charges

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Simplified view of the atom

Page 8: Lecture Ch02

© 2012 Pearson Education, Inc.

How atoms are constructed

Atomic number is the number of protons in an atom’s nucleus

Bonding of atoms • Forms a compound with two or more

elements • Ions are atoms that gain or lose electrons

Isotopes • Have varying number of neutrons

Page 9: Lecture Ch02

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How atoms are constructed

Isotopes • Have different mass numbers – the sum of

the neutrons plus protons • Many isotopes are radioactive and emit

energy and particles

Page 10: Lecture Ch02

© 2012 Pearson Education, Inc.

Minerals

Physical properties of minerals • Habit – common crystal shape• Luster – appearance in reflected light• Color• Streak – color of mineral in powdered form • Hardness – ability to resist scratching or

abrasion• Cleavage – tendency to break along planes

of weak bonding

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Good crystals of the mineral pyrite

Page 12: Lecture Ch02

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Galena displays metallic luster

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Mohs scale of hardness

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Minerals

Physical properties of minerals • Fracture – random pattern of breakage• Specific gravity – mineral density• Other properties

• Taste• Smell• Elasticity• Malleability

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Conchoidal fracture

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Minerals

Physical properties of minerals • Other properties

• Feel• Magnetism• Double Refraction• Reaction to hydrochloric acid

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Minerals

A few dozen minerals are called the rock-forming minerals • The eight elements that compose most

rock-forming minerals are oxygen (O), silicon (Si), aluminum (Al), iron (Fe), calcium (Ca), sodium (Na), potassium (K), and magnesium (Mg)

• Most abundant atoms in Earth’s crust are oxygen (46.6% by weight) and silicon (27.7% by weight)

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Composition of continental crust

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Minerals

Mineral groups • Rock-forming silicates

• Most common mineral group • Contain the silicon-oxygen tetrahedron

(molecule)• Four oxygen atoms surrounding a much smaller

silicon atom

• Combines with other atoms to form the various silicate structures

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The silicate (SiO4)-4 molecule

Page 21: Lecture Ch02

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Minerals

Mineral groups • Rock-forming silicates

• Groups based upon tetrahedral arrangement • Olivine – independent tetrahedra

• Pyroxene group – tetrahedra are arranged in chains

• Amphibole group – tetrahedra are arranged in double chains

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Hornblende – a member of the amphibole group

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Minerals

Mineral groups • Rock-forming silicates

• Groups based upon tetrahedral arrangement • Micas – tetrahedra are arranged in sheets

• Two types of mica are biotite (dark) and muscovite (light)

• Feldspars – Three-dimensional network of tetrahedra

Page 24: Lecture Ch02

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Minerals

Mineral groups • Rock-forming silicates

• Groups based upon tetrahedral arrangement • Feldspars – most abundant group of minerals in

Earth’s crust

• Quartz – three-dimensional network of tetrahedra

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Potassium feldspar

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Minerals

Mineral groups • Nonsilicate minerals

• Major groups• Oxides

• Sulfides

• Carbonates

• Halides

• Native elements

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Common nonsilicate mineral groups

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Minerals

Mineral groups • Nonsilicate minerals

• Carbonates• A major rock-forming group

• Found in the rocks limestone and marble

• Halite and gypsum are found in sedimentary rocks

• Many have economic value

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Minerals

Mineral resources • Mineral resources are occurrences of

useful minerals that will eventually be extracted

• Ore deposits are concentrations of metallic minerals that can be mined at a profit

• Economic factors may change and influence a resource

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An underground halite (salt) mine

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End of Chapter 2