3- atoms, elements,minerals

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    , ,minerals and rocks

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    Carbon 12

    6p + 6n + 6e

    Carbon 13

    6p + 7n + 6e

    sotope

    Carbon 14

    6 + 8n + 6eElectron cloud surrounds

    ( isotope )

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    potassium 2%magnesium

    Distribution of elements in the Earths crust

    o ers

    calcium 4%

    sodium 3%

    Iron 6%

    oxygen 47%

    aluminium 8%

    silicon 28%

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    Elements combine to form minerals

    There are 2 main bonding (combination)

    types1 Ionic bondin

    2) Covalent bonding

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    Ionic bondin

    2e + 8e + 7e = 17ee + e + e = e

    8 Electrons in the outer circle makes the atom stable

    NaCl Halite

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    a e a a a e open orma

    (closed format)

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    made of carbon

    Diamond mineral made of carbon

    bonding

    Ionic

    Covalentbonding

    on ng

    Covalent bondingin all directions

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    4

    pen orma ose orma ym otetrahedron

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    OLIVINE

    Mg

    Fe

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    K K K

    Covalent bonding

    Chain

    K K KK K K Ionic bonding

    Chain

    Covalent bonding

    K K K

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    KK K

    Covalent bondingDouble chain

    Ionic bonding K K K

    Covalent bonding

    K K K

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    Amphibole group

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    .Such zones are called cleavage

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    Pyroxene minerals

    e.g. A u g i t e

    mp oe mneras

    eg. H o r n b l e n d e

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    Definition of a mineral: A mineral is a substance, which is

    Naturally occuring Inorganic Solid Crystalline (with a geometric internal structure) With defined chemical composition

    With characteristic physical properties

    If any one of these properties is not present, the substance is called a Mineraloid

    Minerals are distinguished by their special properties, which reflect theirchemical composition and crystallographic structure.

    , , , , ,FRACTURE, LUSTRE, MAGNETISM, and OPTICAL PROPERTIESare the main physical properties used in the identification of minerals.

    Chemical compositions are determined by various chemical analysis methods.

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    MINERALS

    Rock forming minerals Economic minerals MineraloidsSILICATES

    FeldsparQuartz

    NON-

    SILICATES

    Calcite

    ORE

    MINERALS

    Hematite

    NON-

    METALLIC

    MINERALS

    SOLID

    CoalGlass

    FLUID

    PetroleumWater

    AmphiboleBiotiteMuscovite

    GypsumAnhydriteHalite

    ChromitesPyriteChalcopyrite

    Diamondetc etc etc

    Clay minerals

    Galena etc

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    Definition: A rock is a naturally occurring aggregate of

    ONE or MORE minerals.

    GRANITE ( aggregate of quartz, feldspar, mica) MARBLE (aggregate of calcite) LIMESTONE (aggregate of calcite) SANDSTONE (aggregate of quartz) MUDSTONE (aggregate of clay minerals)

    In eolo a rock does NOT have to be solid

    (cemented, consolidated, lithi fied ).

    e.g. SAND is an unconsolidated sedimentary rock,

    MUD is also and unconsolidated rock

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    Rocks are rou ed under 3 ma or Rock families:

    1. IGNEOUS ROCKS: Granite, Basalt, ......etc.

    They are crystallized from a hot liquid, made of

    molten rock (magma).

    2. SEDIMENTARY ROCKS: Sand Sandstone

    Mudstone, Limestone, .....etc.

    They are formed by the physical or

    chemical deposition of materials, which are

    derived from the earlier existing rocks.

    . , , ,

    Gneiss, ....etc.

    They are formed from earlier existing rocks, by

    ,

    FLUIDS (liquids and gasses).

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    Sedimentary rocks

    sea

    Magma Magma forms

    igneous rocks Basin

    Country rocksMetamorphicrocksAltered

    rocks

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    R O C K C Y C L E

    Igneous rockIgneous rock

    Continental crust

    Subcrust

    ASTHENOSPHERE

    s e n o s p e r e

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    ROCK CYCLE

    Legent

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