Aggradation

Aggradation (or alluviation) is the term used in geology for the increase in land elevation, typically in a river system, due to the deposition of sediment.Aggradation occurs in areas in which the supply of sediment is greater than the amount of material that the system is able to transport.After millions of years, an aggradational environment will become a sedimentary basin, which contains the deposited sediment, including paleochannels and ancient floodplains.Aggradation can be caused by changes in climate, land use, and geologic activity, such as volcanic eruption, earthquakes, and faulting.In 2009, a report by researchers from the University of Colorado at Boulder in the journal Nature Geoscience said that reduced aggradation was contributing to an increased risk of flooding in many river deltas.
Schematic of sediment accumulation (aggradation) in a river channel. The sediment is brown. The river is flowing on bedrock in the upper image, but because sediment was deposited over time the riverbed has risen. This has caused the house to be buried in the lower image.
geologydepositiontransportExner equationalluvialriversriver deltasalluvial fanssubsidencesedimentary basinpaleochannelsfloodplainsclimateland usevolcanic eruptionearthquakesfaultingfloodplainUniversity of Colorado at BoulderNature GeoscienceAvulsion (river)ProgradationWayback MachineDavid MohrigBBC News OnlineRiver morphologyAlluvial plainDrainage basinDrainage system (geomorphology)EstuaryStrahler number (stream order)River valleyRiver deltaRiver sinuosityAlluvial riversAnabranchBar (river morphology)Braided riverChannel patternCut bankMeanderMeander cutoffMouth barOxbow lakePoint barRiffleRapidsRiparian zoneRiver bifurcationRiver channel migrationRiver mouthSlip-off slopeStream poolThalwegBedrock riverCanyonKnickpointPlunge poolBedformsAntiduneCurrent rippleBase levelDegradation (geology)Erosion and tectonicsRiver rejuvenationDeposition (geology)Hack's lawHelicoidal flowPlayfair's lawSediment transportList of rivers that have reversed directionstreamsspringsAlluvial riverBlackwater riverChannelChannel typesConfluenceDistributarySubterranean riverRiver ecosystemRiver sourceTributaryArroyoBourneChalk streamCouleeCurrentStream bedStream channelStreamflowStream gradientPerennial streamWinterbourneEstavelle/InversacGeyserHoly wellHot springlist in the USKarst springMineral springRhythmic springSpring horizonSedimentary processeserosionAbrasionBed loadBed material loadGranular flowDebris flowDissolved loadDowncuttingHeadward erosionPalaeochannelRetrogradationSaltationSuspended loadWash loadWater gapAlluvial fanAntecedent drainage streamAvulsionBillabongFloating islandFluvial terraceMeander scarRiffle-pool sequenceRavineRiver islandRock-cut basinSedimentary structuresStrathInternational scale of river difficultyLog jamStream captureWaterfallWhitewaterSurface runoffAgricultural wastewaterFirst flushUrban runoffFloodsstormwater100-year floodCrevasse splayFlash floodUrban floodingNon-water floodFlood barrierFlood controlFlood forecastingFlood-meadowFlood pulse conceptFlooded grasslands and savannasInundationStorm Water Management ModelReturn periodEffluentIndustrial wastewaterSewageBaer's lawBaseflowBradshaw modelDischarge (hydrology)Drainage densityGroundwater modelHjulström curveHydrographHydrological modelHydrological transport modelInfiltration (hydrology)Main stemRelief ratioRiver Continuum ConceptRouse numberRunoff curve numberRunoff model (reservoir)Stream gaugeUniversal Soil Loss EquationWAFLEXWetted perimeterVolumetric flow rateRiver engineeringAqueductBalancing lakeCheck damDrop structureDaylightingDetention basinErosion controlFish ladderFloodplain restorationInfiltration basinRetention basinRevetmentRiparian-zone restorationStream restorationCanyoningFly fishingRaftingRiver surfingRiverboardingStone skippingTriathlonWhitewater canoeingWhitewater kayakingWhitewater slalomAquiferAquatic toxicologyBody of waterHydraulic civilizationLimnologyRiver valley civilizationRiver cruiseSacred watersSurface waterWild riverRivers by lengthRivers by discharge rateDrainage basinsWhitewater riversFlash floodsRiver name etymologiesCountries without riverssedimentology