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BOOK DICTIONARY General Dictionary of Geology

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  • 7/28/2019 BOOK DICTIONARY General Dictionary of Geology

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    Genera

    lDictionaryof

    Geology

    AlvaKurniawan,JasmineA.P.,JohnM

    c.Kenzie

    2009byEnvironmentalGeographicStudentAssociation

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    GeneralDiction

    aryofGeology

    3

    Editedby:

    AlvaKurniawan

    Departmentof

    EnvironmentalGeography,GadjahMadaUniversity,Yogyakarta,Indonesia

    and:

    JohnMc.K

    enzie

    Departmentof

    Geology,UniversityofCalgary,C

    algary,Canada

    JasmineAn

    itaPutri

    Departmentof

    Geology,UniversityofMelbourne,Melbourne,Australia

    Specialthanksto:

    RichardA.

    Matzner

    Austin,Texas,UnitedStatesofAmerica

    TokuhideA

    kabane

    KyotoUniversity,Kyoto,Japan

    NadineBar

    low

    UniversityofC

    entralFlorida,Orlando,Florida,UnitedStatesofAmerica

    Copyright2009.Env

    ironmentalGeographicStudentAs

    sociation(EGSA)

    Bulaksumur(postalcode55282),Yogyakarta,Indonesia

    Phone:(0274)920340

    Fax:(0274)589595

    DepartmentofEnviron

    mentalGeography

    GeographyFaculty

    GadjahMadaUniversity

    Yogyakarta,Indonesia

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    GeneralDi

    Tho

    ction

    aryof

    Ge

    sdicti

    eoft

    logynary

    isdict

    Sy

    edic

    at

    onar

    y

    ney

    at

    dtoJ

    contr

    Decem

    smine

    butor

    ber20

    Anita

    hich8

    Putri

    eadin

    4

    s

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    GeneralDiction

    aryofGeology

    5

    Foreword

    Inth

    enameofGodmostgraciousmostmerciful,becauseofH

    issalvationthisdictionary

    canbecompleted.Wefeltsohappybeca

    usewecanfinishthisdiction

    arywithoutanybigtrouble

    althoughwelostoneofourbelovededitors.ThankyouverymuchforMr.TokuhideAkabana,

    Mr.RichardAMatzner,andMrs.Na

    dineBarlowwhichgaveusmotivationtofinishthis

    dictionary.

    The

    subjectsofthisdictionaryaremostofgeologicaltermsbuttherearemanytermsthat

    alsorelated

    withgeophysics,biology,astrophysics,andgeography.Geologyisaninteresting

    subjectink

    nowinghistoryofEarthcreation,creatureevolution,ancientEarthlifeandEarth

    conditionin

    thepast;evenfindmine,coal,alsooildepositbelowEarthsurface.Petrogeologist

    studygeologytofindmine,coal,oroild

    eposit.Geophysicsscientiststudygeologyforrecognize

    thephysicalcharacteristicsofEarthcom

    ponentsuchasmagnetism,

    seismicity,elasticity,Earth

    thermodyna

    mic,byphysicalexperimen

    tsinaspecificgeological

    structurewhichconsistof

    specificrocksandminerals.Biologyscientiststudygeologyfortrac

    ingthehistoricalevolution

    ofcreatureinitsfirstappearanceuntilth

    istime.Geographersalsostu

    dygeologyforrecognizea

    spatialphenomenonofEarthsurfacethatwereformedorinfluencedwithasequencesof

    geologicale

    vent.

    Wehopethisdictionarycanhelp

    muchingivingageneralkn

    owledgeaboutmanyterms

    whichbeingusedingeology.Thereis

    nohumancreationthatperfectintheworldlikethis

    dictionary.

    Weapologizeforanymistakesthatwedidntnotice

    aslongaswewritethis

    dictionarya

    ndwehopethateachmista

    kewhichourmadedidntdisturbthefunctionofthis

    dictionaryasaguidetoknowgeological

    terms.Thankyouverymuch

    forusingthisdictionary.

    Editor

    Yogyakarta,Indonesia

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    GeneralDiction

    aryofGeology

    6

    Contents

    Listofedito

    rs

    ......................................................................................................3

    Dedicationpage

    ......................................................................................................4

    Foreword

    ......................................................................................................5

    Contents

    ......................................................................................................6

    A

    ......................................................................................................8

    B

    ......................................................................................................10

    C

    ......................................................................................................13

    D

    ......................................................................................................15

    E

    ......................................................................................................18

    F

    ......................................................................................................20

    G

    ......................................................................................................22

    H

    ......................................................................................................24

    I

    ......................................................................................................26

    J

    ......................................................................................................28

    K

    ......................................................................................................29

    L

    ......................................................................................................30

    M

    ......................................................................................................32

    N

    ......................................................................................................35

    O

    ......................................................................................................37

    P

    ......................................................................................................39

    Q

    ......................................................................................................42

    R

    ......................................................................................................43

    S

    ......................................................................................................46

    T

    ......................................................................................................50

    U

    ......................................................................................................53

    V

    ......................................................................................................54

    W

    ......................................................................................................56

    X

    ......................................................................................................57

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    GeneralDiction

    aryofGeology

    7

    Y

    ......................................................................................................58

    Z

    ......................................................................................................59

    References

    ......................................................................................................60

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    GeneralDiction

    aryofGeology

    8

    AAa:

    AtermofHawaiianorigin.Usedinreferencetoabas

    altic

    lavathatoccursinflowswithafissured,roughandjagged

    surface.

    AcidicRock:

    Anigneousrock

    thathasarelativelyhighsilicacontent.

    Examplesaregraniteandrhyolite.Alsoseeentries

    for

    basic,intermedia

    teandultrabasicrocks.

    AcreFoot:

    Thevolumeofw

    aterneededtofloodoneacreofland

    toa

    depthofonefoot.Equivalentto43,560cubicfeet,1,233

    cubicmetersor325,851gallons.Oneofthemostcommon

    unitsofmeasure

    usedforreservoircapacity.Alsouse

    din

    mineralresourcecalculations(anacrefootofcoal

    isa

    blockofcoalone

    acreinareaandonefootthickitwe

    ighs

    approximately1,800tons).

    Alkali:

    Usedinreferencetomaterialsthatarerichinsod

    ium

    and/orpotassium

    .

    AlluvialFa

    n:

    A

    fanshaped

    wedge

    of

    sediment

    that

    typically

    accumulateson

    landwhereastream

    emergesfrom

    a

    steepcanyonontoaflatarea.Inmapviewithasthesh

    ape

    ofanopenfan.T

    ypicallyformsinaridorsemiaridclima

    tes.

    Alluvium:

    An

    unconsolidated

    accumulation

    ofstreamdepos

    ited

    sediments,includingsands,silts,claysorgravels.

    AngleofRepos

    e:

    Themaximum

    angleth

    atasoil,sedimentorotherloose

    materialcanbeplaced

    oraccumulateandbestable.The

    angleofreposevariesf

    ordifferenttypesofmaterialsand

    differentmoistureconditions.

    AngularUnconformity:

    Anerosionalsurfacethatseparatesrockunitsofdiffering

    dips.The

    rocks

    below

    the

    surface

    were

    deposited,

    deformedanderoded.Theyoungerrocksabovethen

    accumulateduponthee

    rosionalsurface.

    Anthracite:

    Thehighestrankofcoa

    l.Bydefinition,acoalwithafixed

    carboncontentofover91%

    onadryashfreebasis.

    Anthracite

    coalshave

    abrightluster,break

    with

    a

    conchoidalfracture,asemimetalliclusterandaredifficult

    toignite.Frequentlyre

    ferredtobythelaymanas"hard

    coal".

    Aquiclude:

    Asubsurfacerock,soilo

    rsedimentunitthatdoesnotyield

    usefulquantiesofwater.

    Aquifer:

    Asubsurfacerockorsedimentunitthatisporousand

    permeable.Tobeanaq

    uiferitmusthavethesetraitstoa

    highenoughdegreeth

    atitstoresandtransmitsuseful

    quantitiesofwater.

    Aquifer(artesian):

    An

    aquifer

    that

    is

    bounded

    above

    and

    below

    by

    impermeablerockors

    edimentlayers.Thewaterinthe

    aquiferisalsounder

    enoughpressurethat,whenthe

    aquiferistappedbya

    well,thewaterrisesupthewell

    boretoalevelthatisabovethetopoftheaquifer.The

    watermayormaynotflowontothelandsurface.

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    GeneralDiction

    aryofGeology

    Aquifer(confined):

    An

    aquifer

    tha

    tis

    bounded

    above

    and

    below

    by

    impermeablerockorsedimentlayers.Theremayormay

    notbeenough

    pressureintheaquifertomakeitan

    "artesianaquifer".

    Aquifer(unconfined):

    Anaquiferthat

    isnotoverlainbyanimpermeablerock

    unit.The

    waterin

    thisaquiferisunderatmosph

    eric

    pressureandisrechargedbyprecipitationthatfallson

    the

    landsurfacedirectlyabovetheaquifer.

    Arkose:

    Asandstonethatcontainsatleast25%

    feldspar.Easily

    recognizedbecausethefeldspargrainsaretypicallypink

    andangularinsh

    ape.

    Arroyo:

    Aflatbottomgullywithsteepsidesthatisachannelfo

    ran

    intermittentstream.

    Asthenosp

    here:

    Aportionofthe

    uppermantlethatisdirectlybelow

    the

    lithosphere.Azoneoflowstrengthintheupperma

    ntle

    definesthetop

    oftheasthenosphere.Thisweakzone

    allowstheplates

    ofthelithospheretoslideacrossthe

    top

    oftheasthenosp

    here.

    Astroblem

    e:

    AnancientcircularscaronEarth'ssurfaceproducedby

    the

    impactofameteoriteorcomet.UseourGooglem

    aps

    pagetogetclo

    seupimagesofthesemeteorimpact

    structures.

    Atoll:

    Aringshapedgr

    oupofcoralislandsthataresurroun

    ded

    bydeepoceanw

    aterandthatencloseashallowlagoon

    .

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    GeneralDiction

    aryofGeology

    BBackwash:

    Theseawardrushofwaterdownabeachthatoccurswith

    arecedingwave.

    BandedIro

    nOre:

    Arockthatconsistsofalternatinglayersofchertand

    iron

    oxidemineral(u

    suallyhematite)withtheironoxidein

    highenoughconcentrationtobeofeconomicvalue.

    BankfullStage:

    Aheightofwat

    erinastream

    thatcompletelyfills

    the

    naturalchannel.

    Ifthewaterrisesanyhigheraflood

    will

    occur.

    BankStora

    ge:

    Waterthatseep

    sintothegroundalongthebanksofa

    stream

    duringa

    timeofhighflow.Thislossofwater

    into

    thegroundslightlyreducestheheightthatthestream

    will

    attainandthen

    slowlyseepsintothestream

    asthehigh

    waterlevelsubsideshencetheterm"bankstorage".

    Bar:

    Anunderwaterridge,usuallyofsandand/orgravel,

    that

    formsfromthed

    epositionandreworkingofsediment

    sby

    currentsand/or

    waves.Barsoccurinrivers,rivermouths

    andinoffshorew

    aters.

    Barchan:

    Asanddunethatiscrescentshapedinmapview.Barc

    han

    dunesform

    ina

    reasoflimitedsandsupply.Theym

    ove

    acrossthedesertfloorwiththeirgentlyslopingconvex

    sidesfacingupwindand

    theirsteeplyslopingconcavesides

    facingdownwind.

    BarrierIsland:

    Along,narrowislandthatparallelsashoreline.

    Basalt:

    A

    darkcolored

    fineg

    rained

    extrusive

    igneous

    rock

    composedlargelyofplagioclasefeldsparandpyroxene.

    Similarincompositiontogabbro.Basaltisthoughttobe

    oneofthemaincompon

    entsofoceaniccrust.

    BaseFlow:

    Waterthatseepsintoa

    streamthroughapermeablerock

    orsedimentunitthato

    utcropsinthebottomorbanksof

    thestream.

    BaseLevel:

    Thelowerlimitoferosionbyastream.Sealevelisthe

    ultimate

    base

    level.However,lakescan

    serve

    asa

    temporarybaselevelin

    upstreamareas.

    Basement:

    Theigneousandmetam

    orphicrocksthatexistbelowthe

    oldestsedimentarycov

    er.Insomeareassuchasshields

    thebasementrocksmay

    beexposedatthesurface.

    BasicRock:

    Anigneousrockthath

    asarelativelylow

    silicacontent.

    Examplesaregabbroandbasalt.Alsoseeentriesforacidic,

    intermediateandultrabasicrocks.

    Basin:

    Intectonics,acircular,s

    ynclinelikedepressionofstrata.In

    sedimentology,the

    siteofaccumulation

    ofa

    large

    thicknessofsediments.

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    GeneralDiction

    aryofGeology

    Batholith:

    Averylargeintrusiveigneousrockmassthathasb

    een

    exposedbyerosionandwithanexposedsurfaceare

    aof

    over100square

    kilometers.Abatholithhasnoknown

    floor.

    Bathymetry:

    Themeasuremen

    tofoceandepthsandthepreparatio

    nof

    topographicmap

    softheoceanfloor.

    Bauxite:

    Theprincipaloreofaluminum.Amixtureofaluminum

    oxidesandhydroxidesthatformsfrom

    intensechem

    ical

    weatheringofas

    oilintropicalenvironments.

    Bedding:

    Thecharacteristicstructureofsedimentaryrocksinwhich

    layersofdifferen

    tcomposition,grainsizeorarrangem

    ent

    arestackedone

    ontopofanotherinasequencewith

    oldestatthebottomandyoungestatthetop.

    BeddingPlane:

    Adistinctsurfac

    eofcontactbetweentwosedimen

    tary

    rocklayers.

    BedLoad:

    Thelarger,heavierparticlesthatarebeingtransportedby

    astream.Insteadofbeingdissolvedorsuspended,these

    arebeingrolled

    orbouncedalong,spendingatleastpart

    oftheirtimeinc

    ontactwiththestreambottom.Seealso:

    load,suspended

    load,dissolvedload.

    Bedrock:

    Solidrockprese

    ntbeneathanysoil,sedimentorother

    surfacecover.Insomelocationsitmaybeexposedat

    Earth'ssurface.

    BetaParticle:

    Anelectronemittedwithhighenergyandvelocityfrom

    thenucleusofanatomduringradioactivedecay.

    Bhorizon:

    Alayerinthesoil,belo

    wtheAhorizon,wherematerials

    leachedfromaboveacc

    umulate.Typicallyenrichedinclay

    andoxides.

    BiochemicalRo

    cks:

    Asedimentaryrockthat

    formsfromthechemicalactivities

    oforganisms.Organic(reefandfossiliferous)limestones

    andbacterialironoresa

    reexamples.

    Bioturbated:

    An

    adjective

    used

    in

    reference

    to

    a

    sediment

    or

    sedimentary

    rock.Bio

    turbated

    sediments

    have

    been

    disturbedbyanimals(s

    uchasburrowingwormsorshell

    fish)orplantroots.The

    sehavepenetratedthesediment

    anddisturbedanyoralloriginalsedimentarylaminations

    andstructures.Bioturbatedrocksweredisturbedinthis

    way

    while

    stillin

    the

    softsedimentphase

    oftheir

    formation.

    BituminousCoal:

    Arankofcoalthatfallsbetweenanthraciteandsemi

    bituminous.Themostabundantrankofcoal.Frequently

    referredtobythelayma

    nas"softcoal".

    BlockFaultMountain:

    Alinearmountainthatisboundedonbothsidesbynormal

    faults.

    Blowout:

    Ashallow,roundortro

    ughshapeddepressioninsandor

    drysoilthatisformedbywinderosion.Thematerial

    removed

    by

    the

    wind

    may

    also

    be

    referred

    to

    as

    "blowout".

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    GeneralDiction

    aryofGeology

    Butte:

    Aconspicuoushillwithsteepsidesandaflattop.The

    top

    isusuallyacaprockofresistantmaterial.Thisstructureis

    frequentlyaner

    osionalremnantinanareaofflatlying

    sedimentaryrock

    s.

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    aryofGeology

    CCaldera:

    Alarge,bowlsh

    apedcraterassociatedwithavolcanic

    vent.Acaldera

    canform

    from

    avolcanicblastor

    the

    collapse

    ofa

    v

    olcaniccone

    into

    an

    emptied

    magma

    chamber.

    Carbonate

    Rock:

    Arockmadeupprimarilyofcarbonateminerals(mine

    rals

    containingtheCO

    3anionicstructure).Limestone(madeup

    primarilyofcalicite

    CaCO3)anddolostone(made

    up

    primarilyofdolomiteCaMg(CO3)2arethemostcommon

    examples.

    CarbonicA

    cid:

    Aweakacid(H2C

    O3)thatformsfromthereactionofwater

    and

    carbondioxide.Mostrain

    waterisaveryw

    eak

    carbonicacidsolutionformedbythereactionofrainwith

    smallamountsofcarbondioxideintheatmosphere.

    Cataclastic

    Rock:

    A

    brecciaofpo

    wderedrockformedbycrushing

    and

    shearingduringtectonicmovements.

    Cement:

    Asolidprecipitateofcalciumcarbonate,silica,ironox

    ide,

    claymineralsorothermaterialsthatformswithinthep

    ore

    spacesofasedim

    entandbindsitintoasedimentaryro

    ck.

    Cementation:

    Theprocessesth

    roughwhichchemicalprecipitatesform

    withinthepores

    pacesofasedimentandhelpbindit

    into

    asedimentaryrock.

    ChemicalSedim

    entaryRock:

    A

    rockthatformsfromthe

    precipitation

    ofmineral

    materialfromsolution.Examplesarechertandrocksalt.

    ChemicalWeat

    hering:

    Thebreakingdownofsurfacerockmaterialbysolutionor

    chemicalalteration.Common

    alteration

    processesare

    oxidationandhydrolysis

    .

    Chert:

    Amicrocrystallineorc

    ryptocrystallinesedimentaryrock

    materialcomposed

    ofSiO2.Occurs

    as

    nodules

    and

    concretionarymassesandlessfrequentlyasalayered

    deposit.

    Chorizon:

    Thelowesthorizonof

    asoilprofile.Itisbelow

    theB

    horizonandismadeupofweatheredbedrock.

    CinderCone:

    Aconeshapedhillthatconsistsofpyroclasticmaterials

    ejectedfromavolcanicvent.

    Cirque:

    Abowlshapeddepressionwithverysteepsidesthatforms

    attheheadofamounta

    inglacier.Formsfromcoldclimate

    weathering

    processes

    including

    frost

    wedging

    and

    plucking.

    Clastic:

    Asedimentaryrock(suc

    hasshale,siltstone,sandstoneor

    conglomerate)orsedim

    ent(suchasmud,silt,sand,or

    pebbles).An

    accumulation

    oftransported

    weathering

    debris.

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    GeneralDiction

    aryofGeology

    Clay:

    Aclasticmineralparticleofanycompositionthathasa

    grainsizesmallerthan1/256mm.Thetermisalsouse

    din

    referencetoabroadcategoryofhydroussilicatemine

    rals

    inwhichthesilicatetrahedronsarearrangedintosheets.

    Coal:

    A

    brown

    orblacksedimentaryrockthatformsfrom

    accumulated

    plant

    debris.A

    combustible

    rock

    that

    containsatleast50%(byweight)carboncompounds.

    CoastalPla

    in:

    Anareaoflow

    reliefalongacontinentalmarginthatis

    underlainbythick,gentlydippingsediments.

    Compactio

    n:

    Acompressionp

    rocessthatreorientsandreshapes

    the

    grainsofasedim

    entinresponsetotheweightofoverlying

    deposits.

    Composite

    Cone:

    Aconeshapedvolcanicmountaincomposedofalterna

    ting

    layersofcindersand

    lava

    flows.Also

    known

    a

    sa

    stratovolcano.

    ConeofDe

    pression:

    A

    coneshaped

    loweringofthewatertablearoun

    da

    producingwell.

    ContactM

    etamorphism:

    Alterationofaro

    ck,mainlybyheat,whichoccursadjacent

    toadike,sill,magmachamberorothermagmabody.

    ContourLine:

    Alineonamapthattra

    ceslocationswherethevalueofa

    variable

    is

    constant.

    Forexample,contourlines

    of

    elevationtracepointso

    fequalelevationacrossthemap.

    Allpointsonthe"tenfoot"contourlinearetenfeetabove

    sealevel.

    ContourMap:

    Amapthatshowsthechangeinvalueofavariableovera

    geographicareathroughtheuseofcontourlines.For

    example,acontourmapofelevationhaslinesthattrace

    pointsofequalelevation

    acrossthemap.Seealso:contour

    lineandtopographicma

    p.

    CubicFeetPerSecond:

    Aunitofmeasurefrequ

    entlyusedtoquantifytherateof

    flowofastream.Itiseq

    ualtoavolumeofwateronefoot

    highandonefootwide

    movingalineardistanceofone

    footinonesecond.

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    GeneralDictionaryofGeology

    DDatum:

    A

    referencelocationorelevationwhichisuseda

    sa

    startingpointfor

    subsequentmeasurements.Sealevelisa

    datum

    forelevationmeasurements.Datumscanalso

    be

    arbitrarysuch

    a

    sthestartingpointforstream

    stage

    measurementso

    rbaseduponaphysicalfeaturesuchas

    thebaseofarockunit.

    DaughterElement:

    Theelementproducedthroughtheradioactivedecayofa

    parentelement.

    DebrisAva

    lanche:

    Thesuddendow

    nslopemovementofrockandsoilo

    na

    steepslope.

    Decollmen

    t:

    Ahorizontaltosu

    bhorizntalfaultorshearzonewithavery

    largedisplaceme

    nt.Therocksabovethefaultmighth

    ave

    beenmovedthousandsofmetersormorerelativeto

    the

    rocksbelow

    the

    fault.Thisoftenproducesasituation

    wheretherocks

    abovethefaulthaveentirelydifferent

    structuresthantherocksbelowthefault.

    Deflation:

    Theremovalofclayandsiltsizeparticlesfrom

    asoilby

    winderosion.Th

    eterm

    canalsobeusedinreferenceto

    theremovalbyw

    indofanyunconsolidatedmaterial.

    Delta:

    Adepositofsedimentthatformswhereastreamente

    rsa

    standingbodyof

    watersuchasalakeorocean.Thename

    isderivedfrom

    theGr

    eekletter"delta"becausethese

    depositstypicallyhavea

    triangularshapeinmapview.

    DendriticDrain

    age:

    Astream

    drainagepatternthatresemblestheveinsofa

    leafinmapview.Occu

    rsmainlywheretherocksbelow

    haveauniformresistanc

    etoerosion.

    DensityCurrent:

    Agravitydrivenflowof

    densewaterdownanunderwater

    slope.Theincreasedde

    nsityofthewaterisaresultofa

    temperaturedifference,increasedsalinityorsuspended

    sedimentload.

    Deposition:

    Thesettlingfrom

    suspensionoftransportedsediments.

    Also,theprecipitationofchemicalsedimentsfrommineral

    richwaters.

    DesertPaveme

    nt:

    Agroundcoverofgranulesizeandlargerparticlesthatis

    typicallyfoundinarida

    reas.Thisgroundcoverofcoarse

    particlesisaresidualdeposit

    formedwhenthewind

    selectively

    removes

    t

    hesand,

    silt

    and

    claysized

    materials.

    Detrital:

    Awordusedinreferencetosedimentsorsedimentary

    rocks

    that

    are

    composed

    of

    particles

    that

    were

    transportedanddeposit

    edbywind,waterorice.

    Diagenesis:

    Allofthechangeswh

    ichhappentoasedimentafter

    deposition,excluding

    weathering

    and

    metamorphism.

    Diagenesisincludesco

    mpaction,cementation,leaching

    andreplacement.

    Diatom:

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    Aonecelledplan

    tthatlivesintheshallowwatersoflakes,

    streamsorocea

    ns.Manyofthesesecreteashellor

    internalpartsco

    mposedofsilica.Diatomscanoccu

    rin

    verylargenumbe

    rsandcanmakesignificantcontributions

    toseafloororlakesediment.

    Diatomite:

    Alightcolored,

    finegrainedsiliceoussedimentaryrock

    thatformsfroma

    sedimentrichindiatomremains.

    DiatomOo

    ze:

    Aseafloorsedim

    entthatconsistsofatleast30%diatom

    remains.

    Differentia

    tedPlanet:

    A

    planetthath

    aslayerscomposed

    ofelements

    and

    mineralsofdifferentdensities.Asanexample,Earth

    isa

    differentiatedplanetbecauseithasametalrichcore,

    surroundedbya

    rockymantle,andcoveredbyacrus

    tof

    lowdensitymine

    rals.

    Dip:

    Theanglethata

    rockunit,faultorotherrockstructure

    makeswithaho

    rizontalplane.Expressedastheang

    ular

    differencebetweenthehorizontalplaneandthestructure.

    Theangleisme

    asuredinaplaneperpendicularto

    the

    strikeoftherock

    structure.

    Discharge:

    Thevolumeofw

    aterinaflowingstream

    thatpassesa

    givenlocationin

    aunitoftime.Frequentlyexpressedin

    cubicfeetper

    second

    orcubic

    metersperseco

    nd.

    Calculatedbyth

    eformulaQ

    =AxVwhereQ

    is

    the

    discharge,Aisth

    ecrosssectionalareaofthechannel

    and

    Vistheaveragev

    elocityofthestream.

    Discontinu

    ity:

    Asurfaceseparatingrocklayersofdifferingpropertiesor

    compositions.(Se

    eseismicdiscontinuity.)

    DissolvedLoad:

    Thedissolvedmaterialb

    eingcarriedbyastream.Seealso:

    load,suspendedload,be

    dload.

    Divide:

    Aridgethatseparatestw

    oadjacentdrainagebasins.

    Dome:

    Anupliftthatisroundo

    rellipticalinmapviewwithbeds

    dippingawayinalldirectionsfromacentralpoint.

    DrainageBasin:

    Thegeographicareatha

    tcontributesrunofftoastream.It

    canbeoutlinedona

    topographicmapbytracingthe

    pointsofhighestelevation(usuallyridgecrests)between

    two

    adjacentstream

    valleys.Also

    referred

    to

    asa

    "watershed".

    DrainageDivide:

    Theboundarybetweentwoadjacentdrainagebasins.

    Drainagedividesareridgecrests(orlessobviouslocations

    whereslopeofthelandscapechangesdirection).Runoff

    producedononesideo

    ftheridgeflowsintostream

    "A"

    andrunoffontheother

    sideoftheridgeflowsintostream

    "B".

    Drawdown:

    Aloweringofthewatertablearoundaproducingwell.The

    drawdownatanygivenlocationwillbetheverticalchange

    betweentheoriginalw

    atertableandthelevelofthe

    watertablereducedbypumping.

    Drift:

    Ageneralterm

    forall

    sedimentarymaterialsdeposited

    directlyfromtheiceorm

    eltwaterofaglacier.

    Drumlin:

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    A

    low,smoothlyrounded,elongatehill.Drumlins

    are

    depositsofcompactedtillthataresculptedbeneath

    the

    iceofaflowingg

    lacier.Thelongaxisofadrumlinparallels

    theflowdirection

    oftheice.

    Dune:

    Amoundorridgeofwindblownsand.Typicallyfoundin

    desertsandinlan

    dfrom

    abeach.Manydunesaremo

    ved

    bythewind.

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    EEarthflow:

    Adetachedmas

    sofsoilthatmovesdownslopeove

    ra

    curvedfailuresu

    rfaceundertheinfluenceofgravity.An

    earthflowismorecomplexthanaslump;ithasahig

    her

    moisturecontentandthemovingmassofsoilhasso

    me

    internalmovementor"flow".Ratesofmovement

    are

    typicallyafewinchesperyearbutfasterratescanoccu

    r.

    Earthquake:

    Atremblingoftheearthcausedbyasuddenreleaseof

    energystoredinsubsurfacerockunits.

    EbbTide:

    Atidalcurrentthatgenerallymovesseawardandoccurs

    duringtheparto

    fthetidecyclewhensealevelisfalling.

    (seealso:floodtide)

    EffluentStream:

    Astreamthatgainswaterfromgroundwaterflow.Th

    ese

    streamsaretypic

    alofhumidclimateswherewatertables

    arehigh.Thedischargeofaneffluentstream

    can

    be

    sustainedbygroundwaterflowforlongperiodsoft

    ime

    betweenrunoffproducingrainfallorsnowmelt.Efflu

    ent

    streamsgenerallyincreaseindischargedownstream

    and

    containwaterth

    roughouttheyear.Theoppositeis

    an

    influentstream.

    ElasticLimit:

    Themaximumstressthatcanbeappliedtoabodywith

    out

    resultinginperm

    anentdeformationtherockrevertsto

    itsoriginalshape

    afterthestressisremoved.Inthecaseof

    afaultorafoldtheelasticlimitisexceededand

    the

    deformationbecomesapermanentstructureoftheroc

    k.

    ElasticReboundTheory:

    Atheorythatexplains

    theearthquakeprocess.Inthis

    theory,slowlyaccumula

    tingelasticstrainbuildswithina

    rockmassoveranextendedlengthoftime.Thisstrainis

    suddenlyreleasedthrou

    ghfaultmovement,producingan

    earthquake.

    Electron:

    A

    subatomicparticle

    with

    a

    negative

    charge

    and

    of

    negligiblemassthatorbitsthenucleusofanatom.

    Elevation:

    Theverticaldistancebetweenmeansealevelandapoint

    orobjecton,aboveorbelowEarth'ssurface.

    Eolian:

    Aterm

    usedinreferenc

    etothewind.Eolianmaterialsor

    structuresaredeposited

    byorcreatedbythewind.

    Eon:

    Themajordivisionsofthegeologictimescale.Eonsare

    dividedintointervalsk

    now

    as"eras".Twoeonsofthe

    geologictimescalearethePhanerozoic(570millionyears

    agotopresent)andtheCryptozoic(4,600millionyearsago

    until570millionyearsago).

    Epicenter:

    ThepointontheEarth's

    surfacedirectlyabovethefocusof

    anearthquake.

    Epoch:

    Asubdivisionofgeologictimethatislongerthananage

    butshorterthanaperiod.TheTertiaryPeriodisdivided

    intofiveepochs.From

    mostrecenttooldesttheyare:

    Pliocene,Miocene,Oligo

    cene,EoceneandPaleocene.

    Era:

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    Asubdivisionofgeologictimethatislongerthanaperiod

    but

    shorter

    th

    anan

    eon.

    Precambrian,

    Paleoz

    oic,

    Mesozoic,andCe

    nozoicaretheerasofthetimescalefrom

    oldesttoyoungest.

    Erosion:

    A

    generalterm

    applied

    to

    the

    wearing

    away

    and

    movementofearthmaterialsbygravity,wind,waterand

    ice.

    Esker:

    Alongwindingridgeofsortedsandsandgravel.Thou

    ght

    to

    beformed

    f

    rom

    sedimentdeposited

    byastre

    am

    flowingwithinor

    beneathaglacier.

    EustaticSe

    aLevelChange:

    Ariseorfallin

    sealevelthataffectstheentireea

    rth.

    Thoughttobecausedbyanincrease/decreasein

    the

    amountofavaila

    blewaterorachangeinthecapacityof

    oceanbasins.

    Evaporatio

    n:

    The

    processof

    liquid

    waterbecoming

    watervapor.

    Includesvaporiza

    tionfrom

    watersurfaces,landsurfa

    ces

    andsnow/icesurfaces.

    Evaporite:

    Achemicalsedim

    entorsedimentaryrockthathasform

    ed

    byprecipitation

    from

    evaporatingwaters.Gypsum,salt,

    nitratesandboratesareexamplesofevaporiteminerals.

    Evapotranspiration:

    Allmethodsofw

    atermovingfromaliquidtowaterva

    por

    innature.Include

    sbothevaporationandtranspiration.

    Exfoliation

    :

    Aphysicalweatheringp

    rocessinwhichconcentriclayers

    ofrockareremovedfrom

    anoutcrop.

    ExpansiveClay

    (ExpansiveSoil):

    Aclaysoilthatexpandswhenwaterisaddedandcontracts

    whenitdriesout.This

    volumechangewhenincontact

    withbuildings,roadwa

    ys,orundergroundutilitiescan

    causeseveredamage.

    Extrusive:

    Igneousrocksthatcrysta

    llizeatEarth'ssurface.

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    FFacies:

    The

    characterist

    icsofa

    rock

    mass

    thatreflect

    its

    depositionalenv

    ironment.Thesecharacteristicsenable

    therockmassto

    bedistinguishedfromrocksdepositedin

    adjacentenvironments.

    Fault:

    Afractureorfrac

    turezoneinrockalongwhichmovem

    ent

    hasoccurred.

    FaultBlockMountain:

    Alinearmountain

    thatisboundedonbothsidesbynor

    mal

    faults.

    FaunalSuc

    cession:

    A

    principleofr

    elativedatingthatisbasedupon

    the

    observedsequen

    ceoforganismsintherockrecord.The

    relative

    age

    of

    two

    rock

    units

    can

    frequently

    be

    determinedbym

    atchingthefossilsfoundinthoserock

    sto

    theirpositionsin

    therockrecord.

    Felsic:

    Aterm

    usedtod

    escribeanigneousrockthathasala

    rge

    percentage

    oflightcolored

    minerals

    such

    asqua

    rtz,

    feldspar,andmuscovite.Alsousedinreferenceto

    the

    magmasfromwh

    ichtheserockscrystallize.Felsicrocks

    are

    generallyrichin

    siliconandaluminum

    andcontainonly

    smallamounts

    ofmagnesium

    and

    iron.Granite

    and

    rhyolite

    are

    exa

    mplesoffelsicrocks.(See

    mafic

    to

    contrast.)

    Fjord:

    Adeep,narrow,steepwalled,Ushapedvalleythatwas

    carvedbyaglacierandisnowoccupiedbythesea.

    Flood:

    Anoverflowofwaterontolandsthatarenormallyabove

    localwaterlevels.Can

    becausedbystream

    discharge

    exceedingthecapacityo

    fthestreamchannel,stormwinds

    andreducedpressuredrawingwaterfromalakeorocean

    ontothecoastline,dam

    failure,lakelevelincrease,local

    drainageproblemsorotherreasons.

    FloodBasalt:

    Asequenceofparallel

    tosubparallelbasaltflowsthat

    wereformedduringageologicallybriefintervaloftime

    andwhichcoveredanextensivegeographicarea.Thought

    tohaveformedfrom

    simultaneousorsuccessivefissure

    eruptions.

    FloodPlain:

    Anareaofalluviumcove

    red,relativelylevellandalongthe

    banksofastream

    that

    iscoveredwithwaterwhenthe

    streamleavesitschanne

    lduringatimeofhighflow.

    FloodStage:

    Awaterheightthatisreachedwhenthedischargeofa

    streamexceedsthecapa

    cityofthechannel.

    FloodTide:

    Atidalcurrentthatgenerallymoveslandwardandoccurs

    duringthepartofthet

    idecyclewhensealevelisrising.

    (Seeneaptideforcontra

    st.)

    FlowingWell:

    Awellthattapsanaquiferthatisunderenoughpressure

    toforcewatertothesur

    face.Causedwhentheaquiferhas

    arechargeareaatahigh

    erelevation.

    FluidInclusion:

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    Asmallamounto

    ffluid(liquidand/orgas)trappedwithin

    arockandwhichisthoughttorepresentthefluidfrom

    whichtherockcrystallized.

    Focus:

    ApointbeneathEarth'ssurfacewherethevibrationsofan

    earthquakearethoughttohaveoriginated.Alsoknownas

    ahypocenter.

    Fold:

    Abendorflexure

    inarockunitorseriesofrockunitsthat

    hasbeencausedbycrustalmovements.

    Foliation:

    Theplanarorlayeredcharacteristicsofmetamorphicro

    cks

    thatareevidence

    ofthepressuresand/ortemperaturesto

    whichtherockw

    asexposed.Thesecanbestructurals

    uch

    ascleavage,text

    uralsuchasmineralgrainflattening

    or

    elongation,orco

    mpositionalsuchasmineralsegregation

    banding.

    Foraminife

    r:

    Agroupofsinglecelledorganisms,mostlymarine,that

    produceacalcium

    carbonateshell.Theirshellscanm

    ake

    upasignificantportionofthecarbonatesedimentinso

    me

    areas.

    Foraminife

    ralOoze:

    Acalcareoussea

    floorsedimentcomposedofforamin

    ifer

    shells.

    ForsetBed

    s:

    Thedistinctlydippingsedimentlayersdepositedon

    the

    frontofaprogra

    dingdeltaorontheleesideofasand

    dune.

    Formation:

    Alaterallycontinuousr

    ockunitwithadistinctivesetof

    characteristicsthatmakeitpossibletorecognizeandmap

    fromoneoutcroporwelltoanother.Thebasicrockunitof

    stratigraphy.

    Fossil:

    Remains,imprintsortracesofanancientorganism

    that

    havebeenpreservedintherockrecord.Bones,shells,

    casts,tracksandexcrementcanallbecomefossils.

    Fossilfuel:

    Acarbonrichrockmate

    rialorfluid,oforganicoriginthat

    canbeproducedandburnedasafuel.Coal,oilandnatural

    gasareexamplesoffossilfuels.

    Fumarole:

    Aventthatemitshotgases,usuallyassociatedwithpastor

    currentmagmaticactivitybelow.

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    GGabbro:

    Ablack,coarseg

    rainedintrusiveigneousrockthatis

    the

    compositionalequivalentofbasalt.Composedofcalcium

    rich

    feldspars,

    pyroxene

    and

    possibly

    olivine,

    but

    containinglittleif

    anyquartz.

    GageHeight:

    Ameasuredheig

    htofwateraboveareferencedatum.

    Frequentlyused

    todescribetheheightofwaterina

    stream,lake,well,canalorotherwaterbody.

    GagingStation:

    Afacilityonastream,lake,canal,reservoirorotherwater

    bodywhereinstrumentsareinstalledtoautomatic

    ally

    monitorthewate

    r.Measurmentssuchasstage,discharge,

    watertemperatu

    reandpHareautomaticallytakenand

    transmitted

    to

    hydrologists

    via

    satellite,

    radio

    or

    telephone.Measurementsfrom

    thesestationsareuseful

    forawidevariety

    offloodprediction,watermanagement,

    recreationandna

    vigationpurposes.

    Geochrono

    logy:

    Astudyofthetimerelationshipsofrockunits.Inclu

    des

    methodsofbothrelativeandabsolutedating.

    Geomorph

    ology:

    The

    science

    of

    Earth's

    landforms,their

    description,

    classification,dist

    ribution,originandsignificance.

    Geosynclin

    e:

    AmajortroughordownwarpoftheEarth'scrust,inwhich

    greatthicknessesofse

    dimentaryand/orvolcanicrocks

    haveaccumulated.

    GeothermalGradient:

    Theprogressiveincreaseoftemperaturewithdepthinto

    theEarth.

    Geyser:

    Ahotspringthatinterm

    ittentlyeruptsasprayofsteam

    andhotwater.Caused

    bytheheatingofgroundwater

    withinaconfinedopenin

    ginhotrock.

    GlacialRebound:

    AverygradualupliftofEarth'scrustthatoccursafterthe

    weightofathickcontin

    entalicesheet(whichproduced

    subsidence)hasmeltedaway.

    GlacialStriation

    s:

    Groovesandscratches

    onabedrocksurfacethatwere

    producedbythemovem

    entofaglacier.Theorientationof

    thestriationsgivesevidencetothedirectionofglacial

    movement.

    GlacialValley:

    AvalleywithaUshapedcrosssectionthatwascutbyan

    alpineglacier.

    Glacier:

    A

    thick

    mass

    ofice

    thatforms

    on

    land

    from

    an

    accumulation

    and

    recr

    ystallization

    ofsnow

    significant

    enoughtopersistthroughthesummerandgrowyearby

    year.Therearetwobasictypesofglaciers:1)valley(or

    alpine)glaciersthatcree

    pdownslopeundertheinfluence

    ofgravity,and2)continentalglaciersthatflowoutward

    fromathickcentralarea

    undertheirownweight.

    Glass:

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    Anamorphous(

    withoutcrystalstructure)igneousr

    ock

    thatformsfrom

    veryrapidcoolingofmagma.Thera

    pid

    coolingdoesnotprovideenoughtimeforcrystalgrowth.

    Gneiss:

    A

    coarsegrained

    ,foliated

    rock

    produced

    by

    regio

    nal

    metamorphism.

    The

    mineralgrainswithin

    gneiss

    are

    elongated

    due

    to

    pressure

    and

    the

    rock

    has

    a

    compositionalbandingduetochemicalactivity.

    Graben:

    Anelongated,downthrownblockboundedbytwostee

    ply

    dippingnormalfaults.Producedinanareaofcru

    stal

    extension.

    GradedBedding:

    Arocklayerthat

    hasaprogressivechangeinparticlesize

    from

    toptobottom.Mostcommonisasequencew

    ith

    coarsegrainsatthebottom

    andfiningupwards,whichis

    typicallycausedb

    yadecliningcurrentvelocitywithin

    the

    depositionalenvironment.

    Granite:

    A

    coarsegrained,intrusive

    igneous

    rock

    compo

    sed

    primarily

    oflightcolored

    minerals

    such

    as

    qua

    rtz,

    orthoclase,sodium

    plagioclase

    and

    muscovite

    m

    ica.

    Graniteisthough

    ttobeoneofthemaincomponentsof

    continentalcrust.

    Gravel:

    Clasticsedimenta

    ryparticlesofanycompositionthat

    are

    over2mmindiam

    eter.

    GravityAnomaly:

    Ageographicareawherethegravitationalattractionis

    significantlyhighe

    rorsignificantlylowerthannormal.

    Greenhous

    eEffect:

    Awarmingoftheatmo

    spherecausedbycarbondioxide

    andwatervaporinthelowerportionsoftheatmosphere

    capturingheatthatis

    radiatedfrom

    andreflectedby

    Earth'ssurface.

    Greenstone:

    Alowgrademetamorphicrockthatfrequentlycontains

    greenmineralssuchaschlorite,epidoteandtalc.

    GroundMorain

    e:

    Ablanketoftillthatisdepositedduringtheretreatofa

    glacier.

    GroundWater:

    Waterthatexistsbelow

    thewatertableinthezoneof

    saturation.Ground

    wa

    termovesslowlyin

    the

    same

    directionthatthewatertableslopes.

    GroundWaterRechargeArea:

    A

    location

    where

    surf

    ace

    waterorprecipitation

    can

    infiltrateintotheground

    andreplenishthewatersupplyof

    anaquifer.

    Guyot:

    Aseamountwithaflatto

    p.

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    HHalfLife:

    Thetimerequiredforonehalfofaradioactivesubstance

    todecayintoitsd

    aughtermaterial.

    HangingValley:

    AtributarytoaUshapedglacialvalleywhich,instead

    of

    enteringthevalle

    yatthesamelevelasthemainstream,

    entersatahigh

    erelevation,frequentlyasawaterfall.

    Thesedifferentstream

    levelsarearesultofthera

    pid

    downcuttingoftheglacierbeingmuchfasterthan

    the

    slowerdowncuttingofthetributarystream.

    HardWate

    r:

    Waterthathasa

    significantamountofdissolvedcalcium

    andmagnesium

    ions.Thiswaterperformspoorlyw

    ith

    mostsoapsanddetergentsandleavesascalydepositin

    containerswhere

    itisheated

    orevaporates.It

    can

    frequentlybeim

    provedthroughtheuseofhomeba

    sed

    watertreatmentsystems.

    Headwater(s):

    The

    upperportionsofa

    drainage

    basin

    where

    the

    tributariesofastreamfirstbeginflow.

    HeatFlow:

    ThemovementofheatenergyfromthecoreoftheEa

    rth

    towardsthesurfa

    ce.

    Hogback:

    Anarrowridgew

    ithsteeplyinclinedsidesofnearlyeq

    ual

    slopes.Formedb

    ydifferentialerosionofsteeplydipp

    ing

    rockunits.

    Hornfels:

    Anonfoliatedmetamorp

    hicrockthatistypicallyformedby

    contactmetamorphisma

    roundigneousintrusions.

    Horst:

    An

    elongatedblockof

    hightopographicreliefthatis

    boundedontwosidesbysteepnormalfaults.Producedin

    anareaofcrustalextension.

    HotSpot:

    Avolcaniccenterlocated

    withinalithosphericplatethatis

    thoughttobecausedbyaplumeofhotmantlematerial

    risingfromdepth.

    HotSpring:

    Anaturalspringthatdeliverswatertothesurfacethatis

    ofhighertemperatureth

    anthehumanbody.

    Humus:

    Thedarkportionofasoilthatconsistsoforganicmaterial

    thatiswellenoughdecayedthattheoriginalsource

    materialcannotbeidentified.

    HydraulicConductivity:

    Theabilityofaporou

    smaterialto

    transmitafluid.

    Permeability.

    Hydrocarbon:

    Anyorganicchemicalco

    mpound(gaseous,liquidorsolid)

    thatiscomposedofca

    rbonandhydrogen.Theterm

    is

    frequentlyusedinrefe

    rencetofossilfuels,specifically

    crudeoilandnaturalgas.

    Hydrograph:

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    Agraphthatshow

    sthechangeofawaterrelatedvaria

    ble

    overtime.Examp

    le:Astreamdischargehydrographshows

    thechangeindisc

    hargeofastreamovertime.

    Hydrologic

    Cycle:

    The

    naturalcycling

    of

    Earth's

    water

    between

    the

    atmosphere,

    su

    rface

    and

    subsurface

    through

    the

    processes

    of

    evaporation,

    transpiration,

    percolation,

    infiltration,runoffandprecipitation.

    Hydrology:

    ThescienceofEarth'swater,itsmovement,abundan

    ce,

    chemistryanddistributionon,aboveandbelow

    Earth's

    surface.

    Hydrolysis:

    Achemicalreactioninvolvingwaterthatresultsin

    the

    breakdownofmineralmaterial.

    Hydrothermal:

    Pertainingtohot

    water,theactionsofhotwateror

    the

    productsproduce

    dbytheactionsofhotwater.

    HydrothermalDeposits:

    Mineraldeposits

    thatareformedbytheactionsof

    hot

    waterorgasesassociatedwithamagmaticsource.

    HydrothermalMetamorphism:

    Alterationofrock

    byhotwatersorgasesassociatedwitha

    magmaticsource.

    HydrothermalVein:

    Adepositofmin

    eralsprecipitatedinafractureby

    the

    actionsofhotwa

    terorgasesassociatedwithamagmatic

    source.

    Hypocenter:

    Apointbeneathearth'ssurfacewherethevibrationsofan

    earthquakearethought

    tohaveoriginated.Alsoknownas

    thefocus

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    IIgneousRo

    ck:

    Arockformedby

    thecrystallizationofmagmaorlava.

    Ignimbrite:

    Anigneousrockformedbythelithificationofashflow

    or

    pyroclasticflowdeposits.

    ImpermeableLayer:

    Alayerofrock,se

    dimentorsoilthatdoesnotallowwa

    ter

    topassthrough.

    Thiscouldbecausedbyalackofp

    ore

    space

    orpore

    spacesthatare

    so

    smallthatwa

    ter

    moleculeshavedifficultypassingthrough.

    Infiltration

    :

    Themovementof

    surfacewaterintoporoussoil.

    InjectionW

    ell:

    Awellthatisusedtoforceafluidintotheground.The

    injectioncouldbedonefordisposalortoplacethefluid

    (suchasnaturalgas)intoasubsurfacereservoir.

    InteriorDrainage:

    Asystemofstrea

    msthatflowintoalandlockedbasinand

    evaporate.

    Intermedia

    teRock:

    Anigneousrockthatha

    sanintermediatesilicacontent.

    Examplesaresyenitea

    nddiorite.Alsoseeentriesfor

    acidic,basicandultrabas

    icrocks.

    Intrusion:

    Aigneousrockbodythatformedfrommagmathatforced

    itswayinto,throughorb

    etweensubsurfacerockunits.

    Intrusive:

    Igneousrocksthatcrysta

    llizebelowEarth'ssurface.

    Ion:

    Anatomorgroupofatomsthathavegainedorlostoneor

    moreelectronandasaresulthasanelectricalcharge.

    IonicBond:

    Achemicalbondforme

    dbytheelectrostaticattraction

    betweenoppositelychargedions.

    IronFormation:

    A

    layered

    deposit

    of

    chemical

    sedimentary

    rocks

    containingatleast15pe

    rcent(byweight)ironintheform

    ofsulfide,oxide,hydroxide,orcarbonateminerals.

    Isograd:

    Alineonamapthat

    representsaspecificdegreeof

    metamorphism.Rockso

    nonesideofthelinehavebeen

    subjectedtoagreaterle

    velofmetamorphismandonthe

    othersideofthelinealo

    werlevelofmetamorphism.

    Isostasy:

    Aconditionofgravitationalbalance(similartofloating)in

    which

    a

    massoflightercrustalrocksare

    buoyantly

    supportedfrombelowbydensermantlerocks.Thecrustal

    rocksabovesubsidein

    tothemantleuntiltheyhave

    displacedanadequate

    amountofmantlematerialto

    supportthem.

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    Isotope:

    Oneofseveralformsofanelement.Thesedifferentforms

    havethesamenu

    mberofprotonsbutvaryingnumbersof

    neutrons.

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    Geology

    JJade:

    Atranslucentge

    mstoneconsistingofeitherjadeite

    or

    nephritethatis

    typicallygreenincolor.Jadeisav

    ery

    durablestonean

    disusedforavarietyofjewelryand

    ornamentalobjec

    ts.Typicallycutinthecabochonshape

    or

    carved.

    Jadeite:

    Ahighpressure

    clinopyroxenethatisfrequentlycarved

    andpolishedasa

    gemstone.

    Jasper:

    Avarietyofcoloredchert,typicallyredorgreenandoften

    foundinassociat

    ionwithironores.Jasperisfrequently

    usedasagemstoneorintheproductionofornaments.

    Jet:

    Avarietyofcoal

    thatisfrequentlycutandpolished

    for

    jewelryorornaments.

    Jetty:

    Ahumanmadestructurebuiltatrightanglestoacoastline

    andextendingintothewater.Jettiesarebuilttoprot

    ect

    anareaofshorelinefrom

    theeffectsofcurrents,eros

    ion

    ordeposition.

    Joint:

    A

    fracture

    in

    rockalong

    which

    there

    hasbeen

    no

    displacement.

    JointSet:

    Agroupofjointsthatar

    eparallelornearlyparallel.They

    arefrequentlyformeda

    tthesametimeintervalfrom

    a

    commonprocess.

    JollyBalance:

    Aspringbalanceused

    inthedeterminationofspecific

    gravity.

    JuvenileWater:

    Waterthatisnew

    tothehydrologiccycle.Broughtto

    Earth'ssurfacethroughv

    olcaniceruptions.

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    ryofGeology

    KKarst:

    A

    landscapetha

    tischaracterized

    bythe

    features

    of

    solutionweatheringanderosioninthesubsurface.These

    featuresinclude

    caves,sinkholes,disappearingstrea

    ms

    andsubsurfacedr

    ainage.

    Kerogen:

    Solidorganicsub

    stancesfrequentlyfoundinshales.The

    organiccomponentofanoilshale.

    Kettle:

    Adepressionformedinglacialdepositswhenabur

    ied

    blockofice,leftbehindbyaretreatingglacier,melts.

    KettleLake

    :

    Alakethatformsinakettle.

    Kfeldspar:

    A

    potassium

    feldsparsuch

    asorthoclase,microcline,

    sanidineoradular

    ia.Alsoreferredtoaspotashfeldspar.

    Kilobar:

    A

    unitofpressure

    equalto

    1000

    bars

    (the

    mean

    atmosphericpressureat100metersabovesealevelisone

    bar).

    Kimberlite:

    Avarietyofperidotitethatisfoundinvolcanicpipeswhich

    arethoughttobeintrusionsfromtheuppermantle.Many

    diamonddepositsarefou

    ndinkimberlitepipes.

    Knickpoint:

    Anabruptchangeinslo

    pe.Apointonastream

    profile

    whereachangeingradientoccurs.Thiscouldbecaused

    byachangeinunderlyingbedrockorbedrockstructure.

    Knob:

    Asmallhilltopthatisrou

    ndinshape.

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    ryofGeology

    LLaccolith:

    Anigneousintrusionthathasbeenforcedbetweent

    wo

    layeredrockunits.Thetopoftheintrusionisarch

    ed

    upwardsandthebottomoftheintrusionisnearlyflat.

    Lahar:

    Amudflowcomp

    osedofwaterandvolcanicash.Lah

    ars

    canbetriggeredbytheflashmeltingofthesnowcapo

    fa

    volcanicmountainorfrom

    heavyrain.Laharsarev

    ery

    dangerousbecausetheycanoccursuddenlyandtravelat

    greatspeeds.

    LaminarFlow:

    Astateofuniform

    flowwithinafluidinwhichthemov

    ing

    particles

    travel

    along

    parallelpaths

    (compare

    w

    ith

    TurbulentFlow).

    Landslide:

    Adownslopemo

    vementofrockandsoiloverafailure

    surface

    and

    und

    erthe

    influence

    ofgravity.Slum

    ps,

    earthflows,debris

    flowsanddebrisslidesareexamples.

    Lapilli:

    Volcanicrockmaterialswhichareformedwhenmagmais

    ejectedbyavolcano.Typicallyusedformaterialthat

    rangesbetween2

    and64millimetersindiameter.

    LateralMoraine:

    Anaccumulation

    oftillalongthesidesofavalleyglacier

    thatisproducedb

    yiceaction.

    Lava:

    MoltenrockmaterialonEarth'ssurface.

    LavaTube:

    Atunnelbelowthesurfaceofasolidifiedlavaflow,formed

    whentheexteriorportionsoftheflow

    solidifyandthe

    molteninternalmaterial

    isdrainedaway.

    Leaching:

    Theremovalofsolublec

    onstituentsfromarockorsoilby

    movinggroundwaterorhydrothermalfluids.

    LeftLateralFau

    lt:

    Afaultwithhorizontalm

    ovement.Ifyouarestandingon

    onesideofthefaultandlookacrossittheblockonthe

    oppositesideofthefaulthasmovedtotheleft.(Alsosee

    RightLateralFault.)

    Levee:

    Alongcontinuousridgebuiltbypeoplealongthebanksof

    astream

    tocontainthe

    waterduringtimesofhighflow.

    Naturalleveescanalso

    bebuiltalongthebanksofa

    stream.Whentheflood

    waterdeceleratesuponleaving

    thechannel,sedimentsq

    uicklydropoutofsuspensionand

    buildaridgeovertime.

    Limb:

    Onesideofafold.The

    dippingrockunitsbetweenthe

    crestofananticlineandthetroughofasyncline.

    Limestone:

    Asedimentaryrockconsistingofatleast50%

    calcium

    carbonate(CaCO2)bywe

    ight.

    Lineament:

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    Astraighttopographicfeatureofregionalextentwhichis

    thoughttorepre

    sentcrustalstructure.Afault,line

    of

    sinkholes,straightstream

    stretchoralineofvolcanoes

    canbeconsidered

    linearfeatures.

    Lithification:

    Theprocessesth

    roughwhichsedimentsareconverted

    into

    sedimentar

    yrock,

    including

    compaction

    a

    nd

    cementation.

    Lithology:

    Thestudyanddescriptionofrocks,includingtheirmine

    ral

    compositionand

    texture.Alsousedinreferencetothe

    compositionaland

    texturalcharacteristicsofarock.

    Lithosphere:

    Therigidoutersh

    elloftheearthwhichincludesthecr

    ust

    andaportionoftheuppermantle.

    LithosphericPlate:

    Alargeslabofthelithospherethatcanbemoved

    by

    convectioncurren

    tmotionwithinthemantle.

    Load:

    Thetotalamount

    ofsedimentbeingcarriedbyastream

    or

    a

    glacier.

    Inclu

    des

    suspended

    materials,

    dissolved

    materialsandmaterialsmovedalongEarth'ssurface.(A

    lso

    see:bedload,dissolvedload,suspendedload.)

    Lode:

    Arichaccumulationofmineralsinsolidrock.Frequentlyin

    the

    form

    ofa

    vein,layeroran

    area

    with

    a

    large

    concentration

    ofdisseminated

    particles.(See

    pla

    cer

    depositforcontra

    st.)

    LongitudinalDune:

    Along,narrow

    sanddunethathasitslongdimension

    orientedparalleltothedirectionofthewind.

    LongitudinalProfile:

    Acrosssectionofastream

    orvalleybeginningatthe

    sourceandcontinuingt

    othemouth.Theseprofilesare

    drawntoillustratethegradientofthestream.

    LongshoreCurrent:

    Aflowofwaterparallel

    toacoastlinethatiscausedby

    wavesstrikingthecoastatanobliqueangle.

    LongshoreDrift:

    Themovementofsedim

    entalongacoastlinecausedby

    wavesstrikingthecoast

    atanobliqueangle.Thewaves

    washsedimentparticles

    upthebeachatanobliqueangle

    andtheswashbacktotheseacarriestheparticlesdown

    thegradientofthebeach.Thisproducesazigzagpathof

    particlemovementalong

    thebeach.

    Lowland:

    A

    relativelyflatareainthelowerlevelsofregional

    elevation.

    LowVelocityZo

    ne:

    A

    zonewithintheupp

    ermantlewhereseismicwave

    velocitiesarerelativelylow.Thiszoneislocatedabout35

    to155milesbelowthesu

    rface.

    Luster:

    Themannerinwhichligh

    treflectsfromamineralsurface.

    Metallic,submetallicand

    nonmetallicarethebasictypes

    ofluster.

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    MMafic:

    Aterm

    usedtodescribeanigneousrockthathasalarge

    percentageofda

    rkcoloredmineralssuchasamphibo

    le,

    pyroxene

    and

    olivine.Also

    used

    in

    reference

    to

    the

    magmasfrom

    wh

    ichtheserockscrystallize.Maficrocks

    aregenerallyrichinironandmagnesium.Basalta

    nd

    gabbro

    are

    examplesofmafic

    rocks.(See

    felsic

    to

    contrast.)

    Magma:

    Moltenrockmate

    rialthatoccursbelowEarth'ssurface.

    MagmaChamber:

    Afulloremptied

    magmareservoirintheshallowportion

    ofthelithosphere

    .

    MagmaticWater:

    Waterthatisdissolvedinamagmaorwaterthat

    is

    releasedfromam

    agma.Somemagmascancontainup

    to

    severalpercentdissolvedwaterbyweight.

    MagneticA

    nomaly:

    An

    increase

    or

    decrease

    in

    the

    localmagneticfield

    comparedtothen

    ormallyexpectedvalue.

    MagneticD

    eclination:

    ThehorizontalangulardifferencebetweenTrueNortha

    nd

    MagneticNorth.

    MagneticInclination:

    Theverticalangulardiffe

    rencebetweenahorizontalplane

    andtheorientationofEarth'smagneticfield.

    MagneticNorth

    :

    Thedirectionthatacom

    passpoints.Thelocationwhere

    Earth'smagneticfielddip

    sverticallyintotheEarth.

    MagneticRever

    sal:

    Achangeinthepolarity

    ofEarth'smagneticfieldinwhich

    thenorthmagneticpolebecomesthesouthmagneticpole

    andviceversa.Alsoknownasgeomagneticreversalor

    polarityreversal.Earth's

    magneticfieldhasreversedmany

    timesinthepastandthetimeintervalsbetweenthese

    changesareknownaspo

    larityepochs.

    MagneticStratigraphy:

    ThecorrelationofrockunitsandstudyofEarth'shistory

    usingmagneticeventsandmagneticepochsasatime

    reference.

    Magnetometer:

    Aninstrumentdesigned

    tomeasurethestrengthand

    characterofEarth'smagn

    eticfield.

    Magnitude:

    Ameasureofearthquake

    strengthbasedupontheamount

    ofground

    motion

    experienced

    and

    corrected

    forthe

    distancebetweentheobservationpointandtheepicenter.

    Thereareseveralmagnitudescalesinuse.

    Manganesenod

    ule:

    Aroundedconcretion,richinmanganesemineralswith

    minorconcentrationsof

    cobalt,copperandnickel.These

    occurinabundanceonsomepartsofthedeepoceanfloor

    and

    have

    been

    considered

    asa

    potentialsource

    of

    manganese.

    Mantle:

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    ryofGeology

    AmajorsubdivisionofEarth'sinternalstructure.Located

    betweenthebase

    ofthecrustandoverlyingthecore.

    MantlePlume:

    Arisingmassofhotmantlematerialthatcancreate

    an

    areaofvolcanic

    activityinthecenterofalithosphe

    ric

    plate.

    Massive:

    A

    term

    used

    in

    reference

    to

    a

    rock

    unitthat

    is

    homogeneousint

    exture,fabricandappearance.

    MassWasting(alsoMassMovemen

    t):

    Ageneraltermusedforanydownslopemovementofro

    ck,

    soil,snoworiceundertheinfluenceofgravity.Includ

    es:

    landslides,creep,rockfallsandavalanches.

    Meanderin

    gStream:

    Astream

    thatha

    smanybends(meanders).Thistype

    of

    drainage

    pattern

    usually

    developson

    a

    nearly

    le

    vel

    landscapeandwherethebanksofthestream

    areeasily

    eroded.

    MechanicalWeathering:

    A

    generalterm

    applied

    to

    a

    variety

    ofweather

    ing

    processesthatresultintheparticlesizereductionofrock

    materialswithno

    changeincomposition.Frostaction,salt

    crystalgrowthandpressurerelieffracturingareexamples.

    Alsoknownasphysicalweathering.

    MedialMoraine:

    Astreakoftillin

    thecenterofaglacier.Thesearefou

    nd

    downslopefrom

    thejunctionoftwoglaciersandarea

    mergingoftheirla

    teralmorainedeposits.

    MedicalGe

    ology:

    Thestudyofhumanhea

    lthrelatedtogeology.Examples

    wouldincludethecorre

    lationofdiseaseorvitalitywith

    residencesoverspecific

    typesofbedrock

    orhealth

    problemsassociatedwithexposuretospecificmineral

    materials.

    Metamorphism:

    Alterationoftheminerals,texturesandcompositionofa

    rockcausedbyexposuretoheat,pressureandchemical

    actions.

    MeteoricWater:

    Waterfrom

    theatmosphere,suchasrain,snow,hail,or

    sleet.

    Meteor:

    A

    meteoroid

    that

    penetrates

    Earth's

    atmosphere,

    producingastreakofbrig

    htlightcausedbyincineration.

    Meteorite:

    Aparticleofironorrock

    thathasfallentoEarth'ssurface

    frominterplanetaryspac

    e.

    Meteoroid:

    Aparticleofironorrockfoundininterplanetaryspace.

    Distinguished

    from

    planetsorasteroidsbyitsmuch

    smallersize.

    Microseism:

    AvibrationoftheEarth

    thatisunrelatedtoearthquake

    activityinsteaditiscau

    sedbywind,movingtrees,ocean

    wavesorhumanactivity.

    Mineral:

    A

    naturallyoccurring,

    inorganicsolid

    with

    a

    definite

    chemicalcompositionandanorderedinternalstructure.

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    Mineralogy

    :

    The

    studyofminerals

    theircomposition,structu

    re,

    formation,uses,

    properties,occurrenceandgeograp

    hic

    distribution.

    MohorovicicDiscontinuity:

    The

    boundary

    b

    etween

    the

    crust

    and

    the

    mantle.

    Frequentlyreferre

    dtoastheMoho.

    MohsHard

    nessScale:

    Acollectionofm

    ineralsrangingfrom

    verysofttovery

    hard.

    Use

    as

    a

    comparison

    scale

    during

    mine

    ral

    identification.Fro

    msoftesttohardest,thetenminerals

    are:talc1,gypsum2,calcite3,fluorite4,apatite

    5,

    orthoclase6,quartz7,topaz8,corundum9,anddiamo

    nd

    10.Developedby

    FriedrichMohs,aGermanmineralogist

    intheearly1800's

    .

    Monocline:

    Anareaofincreas

    eddipinotherwisegentlydippingstra

    ta.

    Moraine:

    Amound,ridgeorgroundcoveringofunstratifieda

    nd

    unsortedtill,depo

    sitedbyiceactionorbymeltingaway

    of

    aglacier.

    Mountain:

    Ageneralterm

    usedinreferencetoanareathatisa

    ta

    conspicuouslyhig

    herelevationthansurroundinglan

    ds.

    Mountainsarelar

    gerthanhillsandaresignificantenou

    gh

    inreliefthattheyaregivennamesbylocalresidents.

    Mudflow:

    Atypeofmassm

    ovementcomposedmainlyofclays

    ize

    materialswithahighenoughwatercontentthatitflo

    ws

    readily.

    Mudstone:

    Asedimentaryrockcom

    posedofclaysizeparticlesbut

    lackingthestratifiedstructurethatischaracteristicofa

    shale.

    M.Y.:

    Millionyearsabbreviation.

    M.Y.A.:

    Millionyearsagoabbreviation.

    Mylonite:

    Abrecciatedmetamorph

    icrockfrequentlyfoundinafault

    zone.Thefracturedtex

    tureisthoughttoform

    bythe

    crushingactionsoffaultm

    ovement.

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    ryofGeology

    NNannofossils:

    Agenerictermus

    edinreferencetoverysmallfossilsthat

    areatthelimitofresolutionbyalightmicroscope.Th

    ey

    arethereforestudiedwithelectronmicroscopesandare

    frequentlyfossildiscoastersandcoccoliths.

    Nappe:

    Alargeslabofea

    rth'ssurfacethathasbeenmovedina

    horizontalornea

    rhorizontaldirectionoveraplane

    of

    separation.Thismotioncanbeproducedbyfaulting

    or

    sliding.Theterm

    isgenerallyusedforverylargeslabs

    whicharemanysq

    uarekilometersormilesinsurfacearea.

    NativeMet

    al:

    Anaturaldepositofametallicelementsuchasgold,silv

    er,

    copperorironina

    pureform.

    NaturalBridge:

    Anarchshapedrockformationproducedbyweathering

    and/orerosion.

    NaturalGas:

    Naturallyoccurrin

    ghydrocarbonsthatexistinsubsurface

    rockunitsinthe

    gaseousstate.Methaneisthemost

    abundantbutethane,propaneandothersalsooccur.

    NaturalLev

    ee:

    Amoundofsedimentthatparallelsastream

    channel

    formingaleveelikedeposit.Whenfloodwatersleavethe

    normalstreamchannelandenterthefloodplainthereisa

    reductionofvelocitythatcausessuspendedsediments

    to

    falltothebottom,producingthisdeposit.

    Neaptide:

    Adailytidalrangeofmin

    imalamplitudethatoccurswhen

    themoonandsunarepositionedat90degreestoone

    another.

    In

    this

    moo

    nearthsun

    configuration,

    the

    gravitationalattractiono

    fthemoonandsuncompetefor

    Earth'swater.Occursatthefirstandthirdquartersofthe

    moon.Seespringtidefor

    contrast.

    Nebula:

    AcloudofinterstellardustthatisfaintlyvisiblefromEarth.

    Neutron:

    Asubatomicparticle,con

    tainedinthenucleusofanatom.

    Ithasnoelectricalcharg

    eandamasssimilartothatofa

    proton.

    Nodule:

    Amineralmassthathasadifferentcompositionorismore

    weatheringresistantthanitssurroundingrock.Theseare

    normally

    rounded

    in

    s

    hape.Examplesinclude:chert

    massesinalimestonerockunit,pyritemassesinacoal

    seam,orcarbonatemass

    esinashale.Inmostcasesthese

    "nodules"haveformedwithintherockunitoritsformer

    sedimentmass.Thete

    rmisalso

    applied

    to

    rounded

    massesofmanganesem

    ineralsthatoccuronsomeparts

    oftheoceanfloor.

    NonPointSourcePollution:

    Pollutionthatdoesnoto

    riginateatasinglelocation.Inan

    urbanarearunoffwater

    canbepollutedasitflowstoa

    stream

    by

    gasoline,a

    ntifreeze,road

    salt

    or

    other

    contaminants.Inruralareasrunoffcanbecontaminated

    byinsecticides,manure,

    orfertilizer.Thiscontamination

    canbesignificantbutcannotbetracedbacktoaspecific

    source.

    NormalFault:

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    Afaultwithverticalmovementandaninclinedfaultplane.

    Theblockabovethefaulthasmoveddownrelativetothe

    blockbelowthefa

    ult.

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    OObliqueSlipFault:

    Afaultthathasb

    othhorizontalandverticalelements

    of

    displacement.

    Obsidian:

    Aglassyigneousrockwithacompositionsimilartogranite.

    Theglassytexture

    isaresultofcoolingsofastthatmine

    ral

    latticeswerenotd

    eveloped.

    OilField:

    Thegeographicar

    eaaboveanundergroundaccumulation

    ofoilandnaturalgas.

    OilShale:

    Adarkcoloredshalecontaininganunusualamount

    of

    solidorganicmaterial.Thisshalecanbecrusheda

    nd

    heatedtoliberategaseousandliquidhydrocarbons.

    At

    presenttheexpen

    diturerequiredtoprocessoilshaleinto

    a

    fuel

    makes

    this

    effort

    marginally

    profitable

    or

    unprofitable.

    OldAge:

    Astageinthedevelopmentofalandscapewhenstreams

    havealowgradie

    ntandmeanderbackandforthacross

    broadfloodplains.Thelandscapeismarkedbymeander

    scarsandoxbowlakes.

    Oolite:

    Asmallsphereof

    calcium

    carbonatenomorethanafew

    millimetersindiameterandwithaconcentricinternal

    structure.These

    spheresarethoughttohaveformed

    by

    inorganicprecipitationofcalcium

    carbonateinverythin

    layersaroundagrainofs

    andoraparticleofshellorcoral.

    Arockcomposedprimarilyofoolites.

    Oolitic:

    A

    limestonetexturethatischaracterizedbyspherical

    grainsofcalcium

    carbo

    natewithaconcentricinternal

    structure.Thesegrainsa

    rethoughttoform

    byinorganic

    precipitationofcalciumcarbonatearoundasandgrainor

    shellparticlenucleus.

    Opaque:

    Anadjectiveusedinreferencetoasubstancethatdoes

    notallow

    lightofvisiblewavelengthtoenterorpass

    through.Mineralswitha

    metallicorsubmetalliclusterare

    normallyopaque.

    OphioliteSuite:

    Thetypicalsequenceof

    rocksintheoceaniccrust:from

    bottom

    totop:ultrabas

    icrocks,gabbro,sheeteddikes,

    pillowbasalts,andseafloorsediments.Igneousrocksand

    deepseasedimentsassociatedwithdivergencezonesand

    theseafloorenvironmen

    t.

    Orbit:

    Anellipticalorhyperbo

    licpathtraveledbyasatellite

    objectaroundamoremassivebody.Forexample,the

    EarthorbitstheSun.

    OreDeposit:

    Anaturalaccumulation

    ofametal,gemstoneorother

    valuable

    mineralsubstance,which

    isrich

    enough

    in

    concentrationthatitcanbeminedandprocessedata

    profit.

    OreMineral:

    Amineralthatcontainsahighenoughconcentrationofa

    usefulelement

    or

    compound

    that

    the

    element

    or

    compoundcanbeextract

    edataprofit.

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    OriginalHo

    rizontality:

    Oneoftheprinciplesofrelativedating.Baseduponthe

    goodassumption

    thatsedimentaryrocksaredeposited

    in

    horizontalornear

    lyhorizontallayers;thenifsedimentary

    layersarefoundinaninclinedorientationtheforcethat

    movedthemtothatorientationmusthavebeenapplied

    at

    sometimeafterth

    eirdeposition.

    OrogenicBelt:

    Alinearorarcuate

    regionoffoldedandupliftedrocks.

    Orogeny:

    Acompressivete

    ctonicprocessthatresultsininten

    se

    folding,reversefaulting,crustalthickening,upliftandde

    ep

    plutonicactivity.A

    mountainbuildingepisode.

    OscillationRippleMarks:

    Symmetricalridge

    sinsandorothersedimentthatare

    causedbyabackandforthwaveaction.

    Outcrop:

    Anexposureofbe

    drock.Outcropscanbeformednatura

    lly

    or

    by

    human

    a

    ction.Stream

    erosion

    and

    highw

    ay

    constructioncanp

    roduceoutcrops.

    Outfall:

    Alocationwhere

    waterisdischarged.Normallyused

    in

    referencetowhe

    reawatertreatmentfacilityreleases

    treatedwaterinto

    theenvironment.

    Outgassing:

    Thereleaseofju

    venilegasesandwatertothesurfa

    ce

    fromamagmasou

    rce.

    Outwash:

    Sortedandstratifiedse

    dimentdepositedinfrontofa

    glacierbymeltwaterstreams.

    OverturnedFold

    :

    Afoldthathasbothlimbsdippinginthesamedirection,

    resultingfromoneofthoselimbsbeingrotatedthroughan

    angleofatleast90degre

    es.Overturnedfoldsarefoundin

    areasofintensedeform

    ation.Thenameoverturnedis

    givenbecausethestrat

    aononelimbofthefoldare

    "overturned"orupsidedown.

    OxbowLake:

    Acrescentshapedlake

    thatformswhenameandering

    streamchangescourse.S

    uchchangesincoursefrequently

    occurduringfloodeventswhenoverbankwaterserodea

    newchannel.

    Oxidation:

    Achemicalreactioninwhichsubstancescombinewith

    oxygen.Forexample,the

    combinationofironwithoxygen

    toformanironoxide.

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    ryofGeology

    PPahoehoe:

    AHawaiianterm

    foralavaflowthathasasurfaceflow

    structureappeara

    ncethatlookslikecoiledropeorco

    rd.

    Seeaaforcontrast.

    Paleoclimate:

    Theclimateofag

    ivenareaataspecifictimeinthepa

    st.

    Paleoclimatescan

    bereadfrom

    therocksmuchasare

    as

    withdifferenttyp

    esofclimatesproducesedimentsw

    ith

    specificcharacteristicstoday.

    PaleocurrentMap:

    Amapthatshows

    thedirectionsofcurrentsatthetime

    of

    sedimentdeposition.Thesedirectionscanbedetermin

    ed

    throughthestudyofcrossbedding,ripplemarks,tool

    marksandothersedimentarystructures.

    Paleogeogr

    aphicMap:

    A

    map

    thatshows

    the

    distribution

    ofsedimentary

    environmentsataspecifictimeinthepast.Thesema

    ps

    aremadebystud

    yingtherockrecordtocorrelatero

    ck

    unitsthatweredepositedatthesametime,thenrelating

    rockcharacteristic

    stospecificsedimentaryenvironments.

    Paleomagnetism:

    ThestudyofEarth

    'smagneticfieldovertime.Whenrocks

    that

    contain

    magnetic

    minerals

    are

    deposited,the

    character(verticalandhorizontalorientation)ofEarth's

    magneticfieldislockedwithintherocks.Thisinformation

    canbeusedtostudychangesinEarth'smagneticfield

    as

    wellasthemovem

    entofplatesovertime.

    Paleontology:

    Thestudyofancientlifethroughfossils.

    Pangaea:

    Alargecontinentallandm

    assthatexistedfromabout300

    millionyearsagothroughabout200millionyearsago.It

    includedmostoftheco

    ntinentallithospherepresentat

    thattime.Ithassincebr

    okenupandthefragmentshave

    driftedtobecometheconfigurationofEarth'spresentday

    continents.

    Panthalassa:

    Theancientoceanthatsu

    rroundedthePangaealandmass.

    ParentElement:

    Aradioactiveelementthatspontaneouslydecaysintoa

    newsubstance.Theproductofthisdecayisknownasa

    "daughter"element.

    PeakFlow:

    Themaximum

    instantaneousdischargeofastream

    ata

    specificlocation.Correspondstothehigheststageofa

    flood.

    Peat:

    Anaccumulationofunc

    onsolidatedplantdebristhatif

    buried

    and

    preserved

    could

    become

    coal.

    Special

    conditionsarerequiredt

    oaccumulateandpreserveplant

    materials.Theseconditionsaremostoftenfoundina

    marshorswampwhere

    watercoverpreventsoxidation

    andattackbymostorgan

    isms.

    Pediment:

    Abroad,gentlyslopingerosionalsurfaceoflowlocalrelief

    adjacenttoanerodingclifformountainrange.Theareais

    likelycoveredwithsediments.

    Pegmatite:

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    Averycoarsegra

    inedigneousrock,normallyofgranitic

    composition.Typicallyformsduringthefinalstates

    of

    magma

    chamber

    crystallization

    when

    the

    high

    water

    contentsolutionsallowrapidcrystalgrowth.

    PelagicSed

    iment:

    Aoceansediment

    thataccumulatesfarenoughfromla

    nd

    thatdetritalmaterialsareaminorcomponent.The

    se

    sedimentsarelarg

    elycomposedofthetinyshelldebris

    of

    radiolariansandfo

    raminifera.

    PerchedWaterTable:

    Awatertabletha

    tisisolatedfrom

    andhigherthant

    he

    regionalwaterta

    ble.Thiscanoccurwhenahilltop

    is

    underlainbyanim

    permeablerockunit.Infiltratingwaters

    stackupontheimpermeableunit,creatinganisolat

    ed

    watertablethat

    ishigherthanthewatertableoft

    he

    surroundingland.

    Peridotite:

    Adarkcolored,co

    arsegrainedigneousrockthatisma

    de

    upmainlyofolivineandpyroxene,withverylittlequa

    rtz

    orfeldspar.

    Permeability:

    Ameasureofhow

    wellamaterialcantransmitwat

    er.

    Materialssuchasgravel,thattransmitwaterquickly,ha

    ve

    highvaluesofpermeability.Materialssuchasshale,that

    transmitwaterpoorly,havelow

    values.Permeability

    is

    primarilydeterminedbythesizeoftheporespacesa

    nd

    theirdegreeofinterconnection.Permeabilitymeasures

    areexpressedinu

    nitsofvelocity,suchascentimetersp

    er

    second,andassum

    eagradientofoneverticalfootofdr

    op

    perlinearfoot.

    pH:

    Arelativemeasur

    eoftheacidityoralkalinityofawater

    baseduponascalethatrangesbetween0and14with

    7

    beingneutral.ValuesofpHbelow7indicateacidsolutio

    ns

    andvaluesofpHa

    bove7indicatebasicsolutions.

    PhysicalWeathering:

    A

    generalterm

    applied

    to

    a

    variety

    ofweathering

    processesthatresultintheparticlesizereductionofrock

    materialswithnochange

    incomposition.Frostaction,salt

    crystalgrowthandpressu

    rerelieffracturingareexamples.

    Alsoknownasmechanica

    lweathering.

    PlacerDeposit:

    Amassofstreamsedime

    ntthatcontainsaneconomically

    significant

    concentration

    of

    mineral

    particles.

    This

    accumulationofmineralparticlesisaresultoftheirbeing

    ofhighspecificgravity

    orresistanttoabrasion.Gold,

    magnetite,anddiamonds

    canbefoundinplacerdeposits.

    PlateauBasalt:

    Asequenceofparallel

    tosubparallelbasaltflowsthat

    wereformedduringageologicallybriefintervaloftime

    andwhichcoveredanextensivegeographicarea.Thought

    tohaveformedfrom

    simultaneousorsuccessivefissure

    eruptions.

    PointSourcePo

    llution:

    Watercontaminationtha

    tcanbetracedtoasinglepoint.

    Atoxicmaterialspillan

    dasewagedischargepipeare

    examplesofpointsources.

    PolarityEpoch:

    AnintervaloftimebetweenreversalsofEarth'smagnetic

    field.

    PolarityEvent:

    Aspecificeventintheh

    istoryofEarth'smagneticfield.

    Usuallyusedinreference

    toaspecificpolarityreversal.

    PolarityReversa

    l:

    AchangeinthepolarityofEarth'smagneticfieldinwhich

    thenorthmagneticpolebecomesthesouthmagneticpole

    andviceversa.Alsoknownasgeomagneticreversalor

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    magneticreversal.Earth'smagneticfieldhasrevers

    ed

    manytimesinthepastandthetimeintervalsbetwe

    en

    thesechangesare

    knownaspolarityepochs.

    Porosity:

    Thevolumeofporespaceinarock,sedimentorsoil.

    Usuallyexpressed

    asapercentage.Thisporespacec

    an

    includeopenings

    betweengrains,fractureopeningsa

    nd

    caverns.

    PotableWa

    ter:

    Waterthatisofad

    equatequalityfordrinking.

    Pothole:

    Acylindricalorh

    emisphericalholdinthebedrockofa

    stream

    thatisformedfrom

    thecontinualswirlingmotion

    ofsandandgravelbyswirlingcurrents.

    PPM:

    Anabbreviationfo

    rpartspermillion.

    Precipitatio

    n:

    Movementofwaterfromtheatmospheretothelandor

    to

    asurfacewaterbody.Rain,hail,snow,dew,andsleetare

    allexamplesofpre

    cipitation.

    PrimarySeismicWaves:

    Thefastestsetofearthquakevibrationsalsoknownas

    P

    waves.Theymove

    throughtheEarthincompressiona

    nd

    expansionmotions(muchlikesoundwavesmovethrou

    gh

    air).Calledprimarybecausetheyarethefirstrecordeda

    ta

    seismograph.Prim

    arywavesareabletotravelthrou

    gh

    bothsolidsandliquids.

    ProtoSun:

    Anintermediatestageinthedevelopmentofastarin

    whichalargecloudofdu

    standgasesgraduallycondenses

    throughgravitationalactions.

    ProvenReserves:

    Mineraldepositsthath

    avebeen

    explored

    thoroughly

    enoughtobequantifiedb

    utwhicharestillintheground.

    Pumice:

    Avesicularvolcanicglass

    ofgraniticcomposition.Ithasso

    manyvesiclesthatithasaverylow

    specificgravity

    sometimeslowenoughto

    floatonwater.

    Pwave:

    Primaryseismicwaves.

    Thefastestsetofearthquake

    vibrations.Theymoveth

    roughtheEarthincompression

    andexpansionmotions

    (muchlikesoundwavesmove

    throughair).Calledprim

    arybecausetheyarethefirst

    recordedataseismograph.Primarywavesareableto

    travelthroughbothsolids

    andliquids.

    PyroclasticRock

    :

    Arockformedwhensmallparticlesofmagmaareblown

    fromtheventofavolcanobyescapinggas.

    PyroxeneGranu

    lite:

    Acoarsegrainedcontact

    metamorphicrockthatisformed

    athightemperaturesand

    lowpressuresandwhichisrich

    inpyroxeneminerals

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    QQuarry:

    Asurfacemineus

    uallyfortheextractionofconstruction

    stone.

    Quartz:

    Oneofthemostabundantmineralsintheearth'scru

    st.

    HasachemicalcompositionofSiO2andahardness

    of

    seven.Oneofthe

    indexmineralsinMoh'sHardnessSca

    le.

    Occursinsedimentary,metamorphicandigneousrocks.

    QuartzArenite:

    Asandstoneconsistingofatleast95%quartz.

    Quartzite:

    Ametamorphicrockformedbythealterationofsandsto

    ne

    byheat,pressureandchemicalactivity.

    Quartzose:

    Anadjectiveused

    inreferencetoarockthatiscompost

    ed

    primarilyofquartz

    .

    Quicksand:

    Abedofsandthathasahighwatercontent.Thewater

    within

    thesand

    isoften

    flowingthrough

    the

    spac

    es

    betweenthesandgrains.Thiscreatesasoft,fluidlike

    materialthatyield

    seasilytopressureandinwhichhea

    vy

    objectswillsink.

    Quicksilver:

    Anicknamefortheeleme

    ntmercury.

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    RRadialDrainage:

    Adrainagepatter

    ninwhichstream

    channelsrunaw

    ay

    fromacentralhigh

    pointsuchasavolcanoordome.

    Radiolarian

    :

    Agroupofonec

    elledmarineanimalswithasiliceo

    us

    skeleton

    thatoccupiesshallow

    portionsofthewater

    column.Radiolarianshavearangefrom

    Cambrian

    to

    present.

    Radiolarian

    Ooze:

    Adeepseapelagicsedimentthatcontainsatleast30%

    siliceousradiolaria

    nremains.

    RatingCurv

    e:

    Aplotthatshows

    therelationshipbetweenthestagea

    nd

    discharge(streamflow)ofaspecificstream

    ataspecific

    location.Itiscusto

    marytoplotstreamstageontheya

    xis

    oftheplotanddischargeonthexaxis.Theresulting

    relationshipisnormallyacurve.Ratingcurvescanbeus

    ed

    to

    estimate

    discharge

    (which

    istime

    consuming

    a

    nd

    expensivetomeasure)usingasinglestagemeasureme

    nt

    (whichcanbecollectedwithautomaticequipment).T

    he

    principleofaratin

    gcurveenableshydrologiststomonitor

    thedischargeofm

    anystreamssimultaneouslyoncegag

    es

    havebeenplaced

    tocollectandreportthestageoft

    he

    stream.

    ReactionSe

    ries:

    A

    seriesofinter

    actionsbetween

    ameltand

    mine

    ral

    crystalsincontact

    withthemelt.Inareactionseriest

    he

    firstformedcrysta

    ls(highesttemperatureminerals)react

    withthemelttoproduceanewmineral.

    Recharge:

    Wateraddedtoanaquife

    rorotherwaterbody.Anaquifer

    isrechargedbyprecipitationinanareawheretheaquifer

    hasaporousconnectiont

    othesurface.

    RechargeArea:

    Thegeographicareawhere

    waterinfiltratesinto

    the

    groundandentersanaqu

    ifer.

    Recrystallization

    :

    A

    solidstatereactioninwhichtheatomsofexisting

    crystalswithinarockare

    reorganizedinresponsetoheat

    and/orpressure.Therecrystallized

    mineralgrainsare

    typicallylargerinsizethantheoriginalcrystals.

    RectangularDra

    inage:

    A

    drainagepatterninwhichstream

    channelsdevelop

    withinalargescalenetworkofintersectingjoints.This

    drainagepatternischara

    cterizedbyrightanglebendsin

    thechannelsofstreamsa

    ndstreamsthatintersectatright

    angles.

    RecumbentFold

    :

    Anoverturnedfoldthat

    hastwolimbswhicharenearly

    horizontal.

    Refraction:

    Thebendingofaseismic

    waveasitentersamaterialof

    differentdensity,or,the

    bendingofabeam

    oflightasit

    entersamaterialofdiffer

    entrefractiveindex.

    RegionalMetam

    orphism:

    Metamorphism

    across

    a

    broad

    area

    caused

    by

    the

    elevatedtemperaturesandpressuresofplatecollisionor

    deepburial.

    Regolith:

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