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APES Ch. 8 & 9 Flashcards

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9814544018AquifersPermeable layers of rock and sediment that contain groundwater in many small spaces.0
9814544019Unconfined AquiferWater can flow easily in and out of the aquifer. Porous rock covered by soil1
9814544020Confined AquiferAquifers covered by an impermeable and confining layer impeding water flow in or out.2
9814544021Water TableUppermost aquifer layer where water fully saturates the rock or soil.3
9814544022Groundwater RechargeWater from precipitation percolates through soil and into aquifer. If confined, can't recharge.4
9814544023SpringsWater from some aquifers naturally comes up, natural source of freshwater5
9814544024Artesian WellsDrilled hole in a confined aquifer releases pressure and pushes water up.6
9814544025Cone of DepressionArea where there's no longer any groundwater, caused by well overuse, eventually will go dry.7
9814544026Saltwater intrusionLessened pressure from over-pumping so salt water infiltrates and makes well water salty.8
9814544027FloodplainLand adjacent to river where excess water spreads onto.9
9814544028OligotrophicLakes with low productivity because of little nutrients such as phosphorus and nitrogen.10
9814544029MesotrophicLakes with moderate levels of productivity11
9814544030EutrophicLakes with high levels of productivity12
9814544031Impermeable SurfacesPavement, buildings, etc. Doesn't allow water penetration, water then runs into sewers and streams. Excess water causes floods.13
9814544032LeveeEnlarged bank on each side of river to prevent flooding14
9814544033DikesSimilar to levees but to prevent ocean waters from flooding coasts that are under sea level.15
9814544034DamBarrier that runs across a river/stream to control water flow16
9814544035ReservoirLarge body of water stored behind a dam. Held for consumption, generating electricity, flood control, or recreation.17
9814544036Fish LaddersSets of stairs with water flowing over them to have fish migrate despite dams.18
9814544037AqueductsCanals or ditches used to carry water between locations. Transports water to dry areas.19
9814544038DesalinationRemoves salt from salt water to make fresh water.20
9814544039DistillationDesalination method. Seawater flows in, heated to create steam, cool seawater in condensing coil causes steam to condense. Brine and fresh water then flows out.21
9814544040Reverse OsmosisDesalination method. Seawater flows in, pressure applied, water goes through semipermeable membrane, salt can't. Water and brine flows out.22
9814544041Hydroponic AgricultureCultivation under greenhouse conditions with roots in nutrient rich solution, and not soil.23
9814544042Oceanic PlatesLie underneath ocean. Dense and rich in iron24
9814544043Subsurface MiningTunnels within mountain where people go in.25
9814544044Placer MiningProcess of looking for metals and precious stones in river sediments26
9814544045Mountaintop RemovalMiners remove entire top of a mountain with explosives27
9814544046Open pit miningCreate large pit or hole in ground to mine28
9814544047Mining Spoils/TailingsUnwanted waste material created during mining.29
9814544048Strip MiningMinerals close to the surface, remove soil and rock to expose them, then return unwanted waste material.30
9814544049MetalsElements with properties that conduct electricity and heat31
9814544050OresEconomically valuable concentrated accumulations of minerals.32
9814544051Soil DegradationLoss of some or all of the ability of soils to support plant growth.33
9814544052Cation Exchange CapacityAbility of a soil to absorb and release cations. Determined by clay. Higher is better, but higher decreases porosity, therefore, there's a tradeoff.34
9814544053Texture of soilDetermined by percentage of sand, silt, and clay35
9814544054C HorizonLeast weathered. Most similar to parent material36
9814544055B HorizonMineral material, little organic matter37
9814544056E HorizonLeaches organic acids from above layers to B where they accumulate38
9814544057A HorizonTopsoil. Organic material and minerals39
9814544058O HorizonTop layer. Organic horizon and detritus.40
9814544059Parent MaterialRock material underlying a soil41
9814544060SoilMix of geologic and organic components42
9814544061DepositionAccumulation or depositing of eroded material43
9814544062ErosionPhysical removal of rock fragments from a landscape or ecosystem44
9814544063Acid PrecipitationAcid rain. Sulfur Dioxide reacts with water vapor to form sulfuric acid in rain.45
9814544064Chemical WeatheringBreakdown of rocks and minerals by chemical reactions and dissolving of a rocks chemical elements. Alters newly exposed/primary minerals to make secondary minerals.46
9814544065Physical WeatheringMechanical breakdown of rocks and minerals. Water, wind, or temp. Plants or burrowing animals can contribute. Exposing more surface area and makes more vulnerable to more erosion.47
9814544066Metamorphic RocksOther rick types subjected to high temps and pressure causing physical and chemical changes. Pressure creates distorted bands called foliation.48
9814544067Sedimentary RocksForm by sediments like muds, sands, and gravels compressed by overlying sediments. Can be uniform or different. Contains the most fossils.49
9814544068FracturesCracks caused by stress after cooling50
9814544069Igneous RocksForms directly from magma. Classified by composition and mode of formation51
9814544070MineralsSolid, Crystalline, Specific chemical structure, certain formations, uniform52
9814544071Rock CycleConstant formation and destruction of rock.53
9814544072Richter ScaleMeasure of ground movement in an earthquake. Logarithmic scale.54
9814544073EpicenterExact point on Earth's surface directly above where rock ruptures55
9814544074Seismic ActivityAreas with earthquakes and fault activity56
9814544075EarthquakesRocks of the lithosphere rupture unexpectedly along a fault. Common in fault zones.57
9814544076Fault ZonesLarge expanses of rock where movement had occurred where plates meet.58
9814544077FaultFracture in rock across which there is movement59
9814544078Transform Fault BoundaryPlates move sideways past each other.60
9814544079Convergent Plate BoundariesPlates move towards one another. Continental + Continental= Mountains. Oceanic goes under land, forms mountains and volcanos. Oceanic goes under other oceanic.61
9814544080Divergent Plate BoundariesMagma pushes up and out, making new rocks and bringing copper, lead, and silver, however it is deep under ocean.62
9814544081VolcanoVent in Earth's surface. Emits ash, gas, and molten lava. Can be caused by hotspots or convergent plates.63
9814544082SubductionProcess of one plate passing under another.64
9814544083Seafloor SpreadingOceanic plate meet continental. Oceanic pulled under continental. As other plates move apart, rising magma forms new seafloor crust.65
9814544084Continental PlatesLie beneath landmasses. Contains more silicon dioxide. Plates less dense than oceanic.66
9814544085Tectonic cycleSum of the processes that build up and break up lithosphere67
9814544086Theory of Plate TectonicsEarth's lithosphere is divided into plates, most of which are in constant motion68
9814544087Hot SpotsPlaces where molten material from the mantle reaches lithosphere. Causes volcanoes. Also helps create convection cells69
9814544088LithosphereSolid upper mantle and crust. Overlaps with upper mantle. Made of plates with thin layer of soil.70
9814544089AsthenosphereOuter part of mantle. Made of semi-molten, ductile rock.71
9814544090MagmaMolten rock in mantle72
9814544091Core1st and innermost layer. Split into inner and outer. Inner is solid, outer liquid. Made of nickel and iron.73
9814544092MantleMolten rock that slowly circulates in convection cells. 2nd layer from center.74

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