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Published byEvelyn May Modified over 9 years ago
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What is a Mineral?
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What Exactly is a Mineral? Compositionally and physically distinct substance Four criteria to be a true mineral…
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Naturally Occurring Created through natural geologic processes Synthetic diamond: not a mineralRaw diamond: mineral
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Inorganic That is, they do not consist of carbon-hydrogen molecules that may also form crystalline substances through biological processes Sugar: It looks like a mineral, but is it? Nope. Note the C-H bonds.
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Solid Liquid waterSnowflake—frozen water Not a mineral Mineral…believe it or not
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Definite Chemical Composition Minerals are complex assemblages of multiple elements Chemical Formula Types of atoms involved and relative proportions Ex. Quartz Chemical formula SiO 2 Ex #2: Elbaite Chemical formula Na(Li,Al) 3 Al 6 (BO 3 ) 3 Si 6 O 18 (OH) 4
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Elements Pure chemical substance composed of one type of atom (i.e. specific # of protons…) 88 naturally occurring elements Most common (i.e. compose 98% of the earth’s crust—and therefore, minerals) – Oxygen, silicon, aluminum, iron, calcium, magnesium, potassium, and sodium
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Atomic Structure Atom – Basic unit of an element – Very, very, very small (1/10,000,000,000 m) – Nucleus – Protons (+) – Neutrons (neutral) – Electrons (-) – “cloud” surrounding nucleus—exist in “shells” – Mostly empty space
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Visualizing the size of an atom The nucleus is very small compared to the overall size of an atom Imagine 5 ½ football fields (minus end zones) placed end to end (100 yrds long x 160’ wide) Nucleus is like a grain of sand in the middle of them
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It’s All About the Electrons, Baby… A stable atom is one in which the outermost shell of electrons is completely filled Atoms can fill their outer shells by bonding to other atoms – Ionic bonding – Covalent bonding
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Bonding in a [Nut] Shell… Ionic Bonding – Cations (atoms that have lost an electron) are attracted to anions (atoms that have gained an extra electron) – Neutral compounds – Weaker but more common than covalent bonds
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Bonding in a [Nut] Shell… Covalent bonding – Two or more atoms share their electrons, producing the effect of filled outer electron shells – Very strong bond
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Crystalline Structure Arrangement of atoms are – Orderly – Regular – 3-D – Repeating pattern Halite Biotite Fluorite
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Can You Spot the Mineral Wannabes? Pyrite FeS 2 oil Chalcanthite CuSO 4 -5H 2 O Silicon Carbide SiC
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Growing a Mineral Unit cell—smallest unit structure of a mineral Brick Wall example
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Growing a Mineral: Halite Halite unit cell Halite crystal What halite looks like to us
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Identifying a Mineral All minerals have physical and chemical properties that can be easily recognized Direct result of structure and composition Crystal habit Cleavage Fracture Hardness Color Streak Luster
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Cleavage Not the kind you’re thinking of… The tendency of a mineral to break along flat surfaces Governed by bond strength and crystal structure Stronger bonds = poor or no cleavage→
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Oooo…shiny! Luster – The way a mineral reflects light A metallic mineral is said to have a metallic luster Those that do not have a metallic luster (non- metallic) are assigned names that are self- explanatory – Pearly, resinous, earthy, glassy, etc… Pyrite has a metallic luster Quartz has a glassy luster
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School of Hard Knocks… Hardness – Resistance of a mineral to scratching Hardness can be determined by scratching mineral with an object of known hardness Scale—Mohs – Based on 10 minerals: 1 being talc and 10 being diamond
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