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Edward J. Tarbuck & Frederick K. Lutgens
Earth Science, 10e Edward J. Tarbuck & Frederick K. Lutgens
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Minerals: Building Blocks of Rocks Chapter 1
Earth Science, 10e Stan Hatfield and Ken Pinzke Southwestern Illinois College
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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
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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
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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
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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
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Minerals Physical properties of minerals Crystal form Luster Color
Streak Hardness Cleavage
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The mineral quartz often exhibits good crystal form
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Pyrite (fool’s gold) displays metallic luster
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Three examples of perfect cleavage – fluorite, halite, and calcite
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Minerals Physical properties of minerals Fracture Specific gravity
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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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
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The silicate (SiO4)-4 molecule
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Common silicate minerals
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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
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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
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Potassium feldspar
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Plagioclase feldspar
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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
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Minerals Mineral groups Nonsilicate minerals Major groups Sulfates
Carbonates “Native” elements
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Native Copper
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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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Some common non-silicate minerals
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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
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An underground halite (salt) mine
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The Bingham copper mine in Utah
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End of Chapter 1
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