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Earth Materials Minerals: The Crystalline State. Minerals and Mineralogy Mineral Chemistry Atomic Structure of Minerals Minerals as indicators of the environment of their formation. amethyst. diamond. quartz. pyrite. asbestos. Plate boundaries and Earthquakes.
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Earth MaterialsMinerals: The Crystalline State • Minerals and Mineralogy • Mineral Chemistry • Atomic Structure of Minerals • Minerals as indicators of the environment of their formation amethyst diamond quartz pyrite asbestos
Plate boundaries and Earthquakes
Supercontinent and Plate Motion Fig. 2.10
Supercontinent and Plate Motion 56 million years ago
Supercontinent and Plate Motion 120 million years ago
Supercontinent and Plate Motion 200 million years ago
Earth MaterialsMinerals: The Crystalline State • Minerals and Mineralogy (p. 67-69) • Mineral Chemistry (p. 69-74) • Atomic Structure of Minerals (p. 74-77) • Minerals as indicators of the environment of their formation (p. 92) amethyst diamond quartz pyrite asbestos
Definition of a Mineral • Naturally formed (inorganic)
Definition of a Mineral • Naturally formed (inorganic) • Solid
Definition of a Mineral • Naturally formed (inorganic) • Solid • Specific chemical composition • What chemical elements are present and in what proportions
Definition of a Mineral • Naturally occurring (inorganic) • Solid • Specific chemical composition • Crystal Structure • Ordered arrangement of atoms
Definition of a Mineral • Naturally occurring (inorganic) • Solid • Specific chemical composition • Crystal Structure Examples: quartz (SiO2), calcite (CaCO3), halite (NaCl)
Polished section ~1 cm
Thin section under ordinary light Magnetite Feldspar Mica Quartz
What makes each mineral unique?(p.69) • Composition What chemical elements are present and in what proportions • Quartz SiO2 • Olivine (Mg,Fe)2SiO3
Halite (NaCl) What makes each mineral unique?(p.69) • Crystal Structure How are the chemical elements packed together
Extremely soft Both minerals are made of carbon (C) Extremely hard
Atomic Arrangement& Physical Properties 3D framework Sheet structure
Elements and atoms • Chemical Elements most fundamental substance separated by chemical means • Atoms smallest particle of matter retains all properties of an element
Structure of an Atom Fig. 3.1
Ions and Compounds ( p. 54-56) • Ion an atom with excess charge cations H+ anions O2- • Chemical Compound electrically neutral comb. of ions water, H2O H+, H+, O2-
Complex ions • Combination of ions with a charge Si4+, O48- (SiO4)4- Silicate Ion
Transferring Electrons between atoms Ionic Bonding Fig. 3.2
Covalent Bonds in Watersharing electrons between atoms Fig. 3.4
Nature of Bonding and Physical Properties 3D framework Sheet structure Fig. 3.3 and 3.5
The Three States of Matter Solid Gas Liquid Ice in a glacier is a mineral Water in the oceans is not a mineral
The Three States of Water Controlled by temperature and Pressure Box B3.1
low Temp, High Pressure favors solid state General Rule high Temp, low Pressure favors gaseous state In Geology, melting is a changeof state
Crystal Structure of Minerals (p. 74-77) Two factors that control the arrangement of atoms and ions Number of neighboring atoms/ions Size of atom/ion
Packing arrangementPolymorphs(p. 79) Diamond Graphite Compounds that occur in more than 1 crystal arrangement
Size of ions of some geologically important ions Size is based on Charge Fig. 3.8
O2- O2- O2- O2- Si4+ Silicate ion(SiO4)4-
Ionic Substitution Olivine
Ionic Substitution Olivine Ions of Similar Size and Charge can substitute for each other For example
Ionic Substitution Olivine Mg22+(SiO4)4-
Ionic Substitution Olivine Fe22+(SiO4)4- Fe2+-->Mg2+ Natural Olivine: (Mg,Fe)2SiO4
Phase diagram Minerals as indicators of their environments of their formation p. 92 Pressure Fig. 3.31
geotherm Fig. 3.31
Diamonds from the Mantle Fig. 3.31
Snowball Fig. B3.1