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George Mason - GEOL - 102
4/22/11Cenozoic LifeCenozoicEVIDENCE FOR CENOZOICCLIMATE CHANGE Remember in the Cretaceous, climateswere much warmer than today. Although the oceans and atmosphereare affected by the K/T boundary theclimate soon returned to its greenhousestate i
George Mason - GEOL - 102
2/4/11EVOLUTIONLife on EarthTypes of fossilization, againPermineralizationReplacementCarbonizationMolds/casts steinkern Amber Trace fossils Tracks, trails, and burrowsPermineralization Original pore spacesare permeated withgroundwater. Min
George Mason - GEOL - 102
Geologic Time ScalePERIODEPOCHHoloceneNeogeneTertiaryPliocenePaleogenePleistoceneOligoceneMioceneEocenePaleocene0.011.65.323.736.657.8Mesozoic66.4Cretaceous144Jurassic208Triassic245CarboniferousPermianPaleozoicPhanerozoicCen
George Mason - GEOL - 102
Historical GeologyFinal ReviewSpring 2011Current eventsExtinctionKnow 5 largest extinction eventsPermian and Cretaceous extinction eventsMesozoic Tectonics Chapter 13Breakup of PangeaKnow ages of rifting eventsPalisades & Newark formationsDinos
George Mason - GEOL - 102
GeologicTime Scaleagain!Time & GeologyTime v Rock DivisionsEonEraPeriodEpochAgeRock versus TimeEonothemErathemSystemSeriesStageEvolution of geologic time scaleSedgwick and Murchison1Lithology denesComposition of mineral grainsColorTe
George Mason - GEOL - 102
HISTORICAL GEOLOGYGEOLOGY 102, section 002Spring, 2011Instructor: Dr. Stacey Verardosverardo@gmu.edu, 703-993-1045Class hours: Tuesdays and Thursdays 1:30 -2:45pmOffice: David King Hall Room 3037Office Hour: Thursdays, 11am -noonClassroom: Enterpr
George Mason - GEOL - 102
Early ManPrimate groups Prosimmii Tree shrews, lemurs, tarsiers Often nocturnal Anthropoidea Monkeys, apes, humansProsimii & AnthropoideaEarliest primates -Prosimian The earliestrelatives of theprimates werefound in theMesozoic andare simila
George Mason - GEOL - 102
IntroductionTime scaleTime scaleTaxonomicclassicationThis is theversion thatyou will bequizzed on.kingdoms1Factors for fossilization Rapid burial is the best way for successfulfossilization. Most often occur in shallow water with highenergy
George Mason - GEOL - 102
1/18/11HISTORICALGEOLOGYGeology102SowhatisthedierencebetweenGEO101andGEO102? InthisclassyouwilllearnoftheoriginoftheearthandtheevoluJonoftheland,atmosphereandallofitslife. AndthisiswhereyoullneedtolearntheGeologicTimescale. Therewillbeaquizonito
George Mason - GEOL - 102
4/10/11Mesozoic LifeAfter Permian extinction Seas were dominated by an abundance ofmollusks, sea urchins, crustaceans and sh& reptiles. On land, synapsids were replaced byreptiles. crocodiles, turtles, snakes, lizards and dinosaursMesozoicevents
George Mason - GEOL - 102
Mesozoic tectonicsMesozoic era -55-250myrThe breakup of PangaeaRepresents a change tectonically fromcompressional mountain building in theeast and northern parts of the continentto compressional forces on the westernmargin.What was happening ? La
George Mason - GEOL - 102
Rodinia was rifting apartEarly PaleozoicCambrian-SilurianLaurentiaBalticaKazakhstaniaSiberiaChinaGondwana Iapetus Ocean openthen closedRODINIA to PANNOTIANorth America & EuropeCambrianto SilurianDomes and basins1Vendian to OrdovicianCrat
George Mason - GEOL - 102
Late Paleozoic TectonicsLate Paleozoic 410-250 million years ago. Divided into Devonian, Carboniferous,Permian. By the Permian Pangea was assembled. During this time Acadian & Caladonian orogenies Alleghenian & Hercynian orogeniesLatePaleozoicP
George Mason - GEOL - 102
Paleozoic LifeEarly life Fossil record increases with increase infossil hard parts. Vertebrates evolve. Animals move onto land. Vascular plants show up. Also largest mass extinction EVER.Precambrian-Cambrian Invertebrate phylaEarly Cambrian foss
George Mason - GEOL - 102
2/11/11Plate TectonicsJOIDES resolutionP-wavesEARTHQUAKE WAVES P-waves S-waves Surface waves/Long wavesS-waves Oscillate back and forth perpendicular to the directionof wave travel. Change shape of rock. Only in solids. Cause strong movement
George Mason - GEOL - 102
PLEISTOCENE EPOCH1.7myr7 kyr agoExtent of ice during LGMevidenceAn Alps region glaciated valley In 1836 Louis Agassiz, apaleontologist, began to believe thatthe glaciers in the Alps were oncemuch more extensive than today.Glaciated EuropeChanges
George Mason - GEOL - 102
3/3/11Proterozoic2.5bya-540myaProterozoic compared to Archean. Proterozoic has a more modern type ofplate tectonics, sedimentation, and climate. First major Wilson cycle. First large ice age most of Earth cooled. Most BIFs. 42% of Earths history!
George Mason - GEOL - 102
Rocks & MineralsCriteria to be a mineral Occurs naturally as an inorganic solid. Has a specic internal structure. Has a specic chemical composition can exchange occasionally. Has specic physical properties. Minerals can be composed of one element
George Mason - GEOL - 102
Sedimentary ArchivesWhat determines which type ofsedimentary rock forms indifferent environs?Sedimentary EnvironmentsTectonic settingType of rock being weatheredType of transportClimateAmount of pressure & temperatureTimeSedimentary Environment
George Mason - GEOL - 102
Review Sheet for Historical GeologyExam OneSpring 2011Know the TIME SCALEKnow current eventsScience of Historical GeologyChapter 1Scientific MethodUniformitarianismThe 6 KingdomsTaxonomic ClassifiicationsTypes of FossilizationPermineralization
George Mason - GEOL - 102
Review Sheet for Historical GeologyExam TwoCURRENT EVENTSArchean and the Solar System -chapter 8Archean most of Earths History4.6 bya to 700 mya80% of Earths historySolar Nebular HypothesisKnow the planets!Terrestrial & GaseousMeteorites, Astero
George Mason - GEOL - 302
American Mineralogist, Volume 93, pages 16931720, 2008Review PaPeRMineral evolutionRobeRt M. Hazen,1,* DoMinic PaPineau,1 wouteR bleekeR,2 RobeRt t. Downs,3JoHn M. FeRRy,4 tiMotHy J. Mccoy,5 DiMitRi a. sveRJensky,4 anD Hexiong yang3Geophysical Labora
George Mason - GEOL - 306
Thevesoilformingfactors AllinteracttoformthedierenttypesofsoilThevesoilformingfactors Parentalmaterial Canberock Bedrock Residualsoils Transportedmaterialnotinplace TransportedsoilsThevesoilformingfactors LimestonesandstonebasaltThevesoilform
George Mason - GEOL - 306
CATION EXCHANGECAPACITYCLAY MINERALSAnd clay sized fractionThe very very smallveryKaolinite a clay mineral stacks ofhexagonalsheets shownhere are acharacteristicof many clayminerals. Bar is 50m1/1,000,000 m 1/1000 mmhttp:/www.reading.ac.uk
George Mason - GEOL - 306
soilorganicsSpodosolMyakka.TheOcialStateSoilofFloridaAEBhCarbon(cyclelater) dominantlyaddingCtothesoil soweretalkingmoreabouttheupperhorizonAofthesoildominantly.SOMsoilorganicmaFer OrganicmaFerisessenGaltoproducGvesoils improvesphysicala
George Mason - GEOL - 306
MacronutrientsNitrogenxingnodulesh4p:/blog.lib.umn.edu/denis036/thisweekinevoluAon/2007/08/cooperaAon_gets_complex_1.htmlESSENTIALELEMENTS Wearelearningthatsoilsareverycomplexmedium manyreacAonsoccurring thesystemasawholeinaconstantstateofux.Add
George Mason - GEOL - 306
Soil in the newsSome bad- But also some good thingsThe future rests on the soilbeneath our feet.http:/s.ngm.com/2008/09/soil/img/soil-615.jpgPopulation factsPopulationPopulation The world's population will reach 7billion people late this year, a
George Mason - GEOL - 306
SOILORGANICMATTERSOMPeatIsleofLewis,ScotlandSOM EspeciallyinOandA Nutrients Importantfor Supportmicroandmacroorganisms CEC TheyarepartofSOM Holdingwater Tilth. FormaGonofpedsstructure MostofthisnextweekCarboncycle Wewillcoverthisnextweek
George Mason - GEOL - 306
AGoodrichsoilneeds Soil acomplex,breathingen8ty Soil Plants chemistry9macronutrients Neededforplantstogrow C,H,O,N Crucial96%ofaplant K,Ca,Mg,P(phosphorus)S(sulfur)7micoelements Fe,Cl,Mn(Manganese),B(Boron),Cu,Mo(Molybdenum),Zn Lessthan0.010
George Mason - GEOL - 306
SoilPhysicalproper/es.SoilsamplingSoilsampling EarthDay2007 Sunnyside therepresenta5vesoilfortheDistrictofColumbia U.S.Na5onalArboretum.SoilsamplingSoil TextureSoil Texture = %Sand, Silt & Clay in a soil. Soil texture is the single most impor
George Mason - GEOL - 306
GEOLOGY306SOILSCIENCESPRING2011http:/mason.gmu.edu/~jnord/geol306/PREREQUISITE GEOL 101 and CHEM 103 or 211CLASS MEETS Monday 4:30 p.m. to 7:10 p.m. - Enterprise Hall 276Dr. Julia Nord, 3055 David King HallINSTRUCTOREmail Address - jnord@gmu.eduOF
George Mason - GEOL - 306
Soil Taxonomy- more detailsPurpose of Soil Taxonomy:1. Organize knowledge about soils2. Understand relationships among different soils3. Establish groups or classes for practical purposes.a. predicting behaviorb. identifying best usesc. estimating
George Mason - GEOL - 306
Soil solution- Not pure waterWater striderHydrological cycle water in living thingsImportance to plants Maintain turgidity Carry dissolved nutrients Required for Ps Lost in transpiration to cool plant and keep nutrients moving upImportance to p
George Mason - GEOL - 306
ROCKCYCLEIGNEOUSROCKGraniteh*p:/web.uct.ac.za/depts/geolsci/dlr/rocks/gran9.jpg VIOOLSDRIFBATHOLITHSAA1900Ma ADAMELLITE(TwoFeldsparGranite):Orthoclase(phenocrysHc)PlagioclaseQuartzBioHteMagneHteROCK asolidaggregateofoneormoremineralsormineralli
George Mason - GEOL - 306
SEDIMENTARYROCKSWhiteClisofDover(chalk)h5p:/cache.eb.com/eb/image?id=74594&rendTypeId=4RockcycleWEATHERING producessolidparKcles (primaryandsecondary) +ionsinsoluKonTRANSPORTATION movessolidparKcles (primaryandsecondary) +ionsinsoluKonDEPOS
George Mason - GEOL - 306
TwelveSoilordersPicturesfromNRCSNaturalResourcesConserva8onServiceh:p:/soils.usda.gov/technical/classica8on/orders/En8solrecentSoilsthathaveli:leornoevidenceofdevelopmentofpedogenichorizons.Manyaresandyorveryshallow.MountainsetcIncep8solL.Incept
George Mason - GEOL - 306
ROCKCYCLEWEATHERING thephysicalbreakdown(disintegra5on)andchemicalaltera5on(decomposi5on)ofrocksatornearEarth'ssurface Slowbutconstant Plentyof5meSURFICIALorEXTERNALPROCESSES Aectsthetop150feetjust!WEATHERINGsceneryWEATHERINGscenery TheBrides
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