EAPS 100 Study Guide Exam 1Chapters 0, 1, 2, and 5Chapter 0Different Spheres of the Earth (definition, major compositions)-AtmosphereoEnvelope of gas that surrounds earthoElevation of 10,000 km, thins awayoMain components: N2, O2, other gases-GeosphereoSolid earthoTopography: surface features of landoBathymetry: underwater features of land-Hydrosphereo70% of surface is water (96% in oceans)oFresh water – minor on land surface, more groundwater, glaciers at polarregions/high elevations-BiosphereoSurface, can modify the landscapeoVaries spatially and temporallyEnergy and Exchanges-Internal energy:heat, thermal energyoRocks melt, volcanoesoEarth’s interior soft enough to flowRound earth, tectonic activities-External energy:reach surface from outside, mostly sunoWarmoConvection of atmosphere and hydrosphereWinds, currents, wavesEarth’s Interior (structure, features for each layer, continental vs oceanic)-Crust(least dense)oVery thinoOceanic crust: less thick, primarily basalticoContinental crust: thicker, primarily granitic-Mantle(denser)oLargest part of earth in volumeoSolid – hot and soft to flow (like candle)oUpper mantle: moho to 660 km – transition 410-660oLower mantle: 660-2900 km-Core(most dense)oOuter core: liquid, generates magnetic fieldoInner core: solid, over 4,700 C
-Geothermal Gradient:rule of increasing temp with depthLithosphere & Asthenosphere-LithosphereoRigid, can break, can’t flow, shape/size unchanged (ex: box/stick)oCrust & uppermost mantle (outer 100-150 km)-AsthenosphereoPlastic: deformation permanent without breaking, solid but soft, can flow (ex:magma/lava)oPart of mantleoAbility to flow makes all plates tectonic activities possibleChapter 1Mineral Definition-Mineral:naturally occurring inorganic solid that possesses orderly crystalline structureand definite chemical composition-Requirements (determine if mineral is a mineral)oNaturally occurringoSolidoInorganicoOrdered crystalline structureoCharacteristic chemical compositionsMineral Property Definition/Usage-Color:not reliable, huge range, trace impurities-Luster:way mineral surface scatter lightoMetallic lusteroNonmetallic – vitreous (glassy), earthy (dull), pearly, silky, resinous, greasy-Crystal shape:way crystal grows when unobstructedoEarly crystals seed for future growth, encounter other growing crystals, restrictedby space-Streak:color after mineral is powderedoMore reliable, may be different than mineral color, not all produce streak-Hardness:ability of mineral to resist abrasionoMohs Scale of Hardness: rubbing mineral against material of known hardness(scale of 1-10)-Cleavage and fractureoCleavage:tendency of mineral to break along flat parallel surfaces due to weakchemical bondingoFracture:breaks along random, irregular surfacesoNumber of cleavage directions/angles can be 1-4 or 6oConchoidal fractures:special for quartz, no cleavage, breaks along numeroussmall smooth curved surfaces-Other propertiesoReactions to HCI acid Effervesce, bubble
oMagnetismo
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