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Chapter 9 Earths Interior.pptx - Chapter 9: Earth’s...

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Chapter 9: Earth’s Interior
CrustalComposition98.5% of the crust iscomprised of just eightelements.Oxygen is the mostabundant element in thecrust.This reflects theimportance of silicate(SiO4) minerals.Oxygen is large.Itoccupies ~93% ofcrustal volume.
Earth LayersClassified byChemicalCompositionCRUSTis sampled directly by drilling andis studied extensively by seismicanalysis.It is the thin relatively lightweightoutermost layerit is a rigid layermakes up .4% of the earth’s totalmassless than 1% of its volume.The crust is divided into OCEANICCRUST and CONTINENTAL CRUST
Types ofCrustOCEANIC CRUSTMafic composed primarily of BASALT and GABBROwhich is a heavy, dark colored rock composed mostly of oxygen, silicon, magnesium and ironAverage density of approximately 3.0 g/cm3Average thickness of 7-10 kmCONTINENTAL CRUSTFelsic, averagecomposition of GRANITEwhich is a speckled rock composed mainly of oxygen, silicon and aluminumAverage density of approximately 2.7 g/cm3Average thickness of 35-40 km
Earth LayersClassified byChemicalCompositionMANTLEIs the layer beneath the crustMakes up 68.1% of the earths mass and83% of its volumeComposed of oxygen, magnesium andsiliconDensity varies with depth from 3.3-5.5g/cm3with an average being 4.5 g/cm32900 km in thicknessDivisionsUpper Mantle down to a depth of660 kmLower Mantle from 660 km downto 2,900 kmTransition Zone is the sectionbetween 400 km and 660 km deep
Earth Layers Classified by ChemicalCompositionCOREIs the innermost layerMakes up 31.5% of the earths mass and 16% of itsvolumeComposed of 90% iron and nickel along withsilicon, sulfur, and heavy elementsMetallic central zoneAverage density is 13 g/cm33470 km in thicknessDivided into two partsOUTER COREviscous liquid,with a density of11.8 g/cm3Flow generates theEarth’s magnetic fieldINNER COREsolid with a densityof 16 g/cm3
Earth Layers Classified

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Term
Winter
Professor
N/A
Tags
Crust, Structure of the Earth, Mantle, upper mantle

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