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Edward J. Tarbuck & Frederick K. Lutgens

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1 Edward J. Tarbuck & Frederick K. Lutgens
Earth Science, 10e Edward J. Tarbuck & Frederick K. Lutgens

2 Minerals: Building Blocks of Rocks Chapter 1
Earth Science, 10e Stan Hatfield and Ken Pinzke Southwestern Illinois College

3 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 Mineraloid - lacks an orderly internal structure

4 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

5 Periodic table of the Elements

6 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

7 Simplified view of the atom

8 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

9 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

10 Minerals Physical properties of minerals Crystal form Luster Color
Streak Hardness Cleavage

11 The mineral quartz often exhibits good crystal form

12 Pyrite (fool’s gold) displays metallic luster

13

14 Three examples of perfect cleavage – fluorite, halite, and calcite

15 Minerals Physical properties of minerals Fracture Specific gravity
Other properties Taste Smell Elasticity Malleability

16 Conchoidal fracture

17 Minerals Physical properties of minerals Other properties Feel
Magnetism Double Refraction Reaction to hydrochloric acid

18 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)

19

20 Minerals Mineral groups Rock-forming silicates
Most common mineral group Contain the silicon-oxygen tetrahedron Four oxygen atoms surrounding a much smaller silicon atom Combines with other atoms to form the various silicate structures

21 The silicate (SiO4)-4 molecule

22 Common silicate minerals

23 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

24 Hornblende – a member of the amphibole group

25 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

26 Minerals Mineral groups Rock-forming silicates
Groups based upon tetrahedral arrangement Feldspars Two types of feldspar are Orthoclase and Plagioclase Quartz – three-dimensional network of tetrahedra

27 Potassium feldspar

28 Plagioclase feldspar

29 Minerals Mineral groups Rock-forming silicates Nonsilicate minerals
Feldspars are the most plentiful mineral group Crystallize from molten material Nonsilicate minerals Major groups Oxides Sulfides

30 Minerals Mineral groups Nonsilicate minerals Major groups Sulfates
Carbonates “Native” elements

31 Native Copper

32 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

33 Some common non-silicate minerals

34 Minerals Mineral resources Reserves are already identified deposits
Ores are useful metallic minerals that can be mined at a profit Economic factors may change and influence a resource

35 An underground halite (salt) mine

36 The Bingham copper mine in Utah

37 End of Chapter 1


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