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6/11/2013 1 L3 - MINERALS CIVE 430 ENGINEERING GEOLOGY SUMMER 2013 DEFINITION The earth, the other inner planets and the moon are made of ROCKS. Rocks in turn, are made of MINERALS MINERALS are: Solids ; natural compounds AND they have A regular structure made of ATOMS held together by electromagnetic forces A fixed chemical composition.
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    L3 - MINERALS

    CIVE 430 ENGINEERING GEOLOGY

    SUMMER 2013

    DEFINITION Theearth,theotherinnerplanetsandthemoonare

    madeofROCKS. Rocksinturn,aremadeofMINERALS

    MINERALSare: Solids;naturalcompoundsANDtheyhave AregularstructuremadeofATOMSheldtogetherby

    electromagneticforces Afixedchemicalcomposition.

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    WhatisaMineral?

    PeriodicTable http://www.webelements.com/

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    MineralClassificationMineralsofonetypeofatom nativeelements(Augold,Ag silver,Cu copper,)

    MineralswithCationscombinedwiththelarge,negativeions(anions): oxygen(O oxides),sulfur(S sulfides),halogens(Cl,ForBr halides).

    Aniongroupsmadeofoxygen combinedwithcationsofvalency+3orgreater(seeperiodictablenonmetalsofgroups1317):silicates(SiO4),carbonates(CO3)andsulfates(SO4).

    MineralStructureThisarrangement,knownasCrystalStructure isdeterminedby: Theatomsize TheTypesofBonds:ionic,covalent,VanderWaals

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    Howaremineral'sformedinnature? Fromawatersolution.Thechemicalsinthesolutioncome

    fromdissolvingotherminerals.Thesemineralsformatthesurfaceoftheearthaswaterevaporates(sedimentary)orfromhotwaterinsidetheearthasthatwatercools(hydrothermal).

    Fromasilicatemelt. Themeltcomesfrommeltingminerals.Thesemineralsform:Wheremoltenrockcools eitherintheinteriororatthesurface(igneous).

    Byaddingenergytominerals,rearrangetheionsoftheoldstructureandmakeanewone.

    ThesemineralsformInsidetheearthwherehightemperaturesprovidethenecessaryenergy(metamorphic).

    PHYSICALCHARACTERISTICSOFMINERALS

    Color Luster Cleavage Fracture Hardness SpecificGravity Streak

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    PHYSICALCHARACTERISTICSOFMINERALS

    COLOR: Cobalt,Co,produces: violetred Chromium,Cr,produces: orangered Copper,Cu,produces: azureblue Iron,Fe,produces: red Manganese,Mn,produces: pink Nickel,Ni,produces: green Uranium,U,produces: yellow Vanadium,V,produces: Redorange

    PHYSICALCHARACTERISTICSOFMINERALSSTREAK: Colorofthemineralmaybe

    differentthanthecolorofthestreak.Streakisactuallythecolorofthepowderofamineral

    Properwaytotestforstreakistorubamineralacrossatileofwhiteporcelainandtoexaminethecolorofthe"streak"leftbehind

    HEMATITE

    StreakisBloodRED

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    PHYSICALCHARACTERISTICSOFMINERALSSTREAK

    HEMATITE

    Streak is Blood RED

    PHYSICALCHARACTERISTICSOFMINERALSLUSTER

    Descriptionofthewaylightinteractswiththesurfaceofacrystal.Ithasnothingtodowithcolororshape,butisrelatedtotransparencyandsurfaceconditions.

    Dull justanonreflectivesurfaceofanykind Earthy thelookofdirtordriedmud Fibrous thelookoffibers Greasy thelookofgrease Metallic thelookofmetals Pearly thelookofapearl Pitchy thelookoftar Resinous thelookofresinssuchasdriedglueorchewinggum Vitreous simplymeansthelookofglass Waxy thelookofwax

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    PHYSICALCHARACTERISTICSOFMINERALSLUSTER FibrousAsbestos

    CLEAVAGE Crystalcleavageisasmoothbreakproducingwhatappearstobeaflatcrystalface

    cleavageisreproducible thesamemineralwillalwayshavethesamecleavage.

    CALCITECleavageisperfectin3directions,formingrhombohedrons

    PHYSICALCHARACTERISTICSOFMINERALS

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    Cleavage.GemsSalt

    PHYSICALCHARACTERISTICSOFMINERALS

    NoCleavageConcoidalFractureOBSIDIAN

    Salt

    FRACTURE

    PHYSICALCHARACTERISTICSOFMINERALS

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    HARDNESS Hardnessisameasureofthestrength

    ofthestructureofthemineralrelativetothestrengthofitschemicalbonds

    Hardnesscanbetestedthroughscratching.Groovesrequireeitherthebreakingofbondsorthedisplacementofatoms. Ahardmineralcanscratchasoftermineral,butasoftmineralcannotscratchahardermineral.

    TheMohs HardnessScale DiamondMhoHardness=10

    PHYSICALCHARACTERISTICSOFMINERALS

    MhosHardnessScale1. Talc2. Gypsum3. Calcite4. Fluorite5. Apatite6. Orthoclase7. Quartz8. Topaz9. Corundum(rubyandsapphire)10.Diamond

    PHYSICALCHARACTERISTICSOFMINERALS

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    Mhos Scale

    MhosScale

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    DiamondStructure

    Diamond Structure

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    DENSITY SPECIFICGRAVITY Gold caneasilybedistinguishedfrom

    "fool'sgold" byspecificgravityalone SGorGs =Densityofthemineral

    dividedbythedensityofwater TheEarth'scrust,wherewearemost

    likelytocollectmineralsfrom,iscomposedmostlyofthemineralsquartz,calcite andfeldspar. ThesemineralshaveSG'saround2.7

    PHYSICALCHARACTERISTICSOFMINERALS

    Rock Forming MineralsOxides (containing O2-)-SAPPHIRE (Corundum)

    Sulfides (containing S2-)-GALENA

    Sulfates (containing SO42-)-GYPSUM

    Native Elements-SILVER

    Halides (salts)-FLUORITE

    Carbonates (containing CO32-)-CALCITE

    Hydroxides (containing OH-)-MANGANITE

    Phosphates (containing PO43-)-FLUORAPATITE

    SILICATES (containing SiO44-)

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    Rock Forming Minerals

    RockFormingMineralsCarbonates

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    Rock Forming MineralsCarbonates

    Rock Forming MineralsSilicate MineralsForm 95% of the Earth's crust

    >80% of the Earth's mantle

    Why?

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    RockFormingMineralsSilicateMinerals Quartz Feldspars(Orthoclase,Plagioclase) Mica(Muscovite,Biotite) Clay(Kaolinite,Montmorillonite) OlivineAmphibolePyroxine (Groups) Garnet Serpentine

    RockFormingMineralsSilicateStructure

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    RockFormingMineralsSheetStructure Mica

    RockFormingMineralsSilicateMinerals

    Feldspar Mica

    PyroxeneQuartzOlivine

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    RockFormingMineralsNonSilicateMinerals

    Halite Spinel

    CalcitePyriteGalena

    Gypsum

    Hematite