9/18/2012 1 GEOS 302 Rivers & Fluvial Deposits Fluvial Systems River deposystems and their components 1) transport systems 2) zones of accumulation Bow River, Banff Natl. Park A. Cohen Photo Importance of Fluvial Systems Environmental issues: flooding water transport agriculture soil erosion nutrient transport Importance of Fluvial Systems Resource issues -Facies models for hydrocarbon plays and groundwater reservoirs -Sensitivity to changes in climate and tectonics Channeled Scablands WA Megaflood Bedforms Fluvial Channels as Hydrocarbon Reservoirs Sands
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GEOS 302 Rivers & Fluvial DepositsFluvial Systems
River deposystems and their components1) transport systems2) zones of accumulation
Bow River,Banff Natl. ParkA. Cohen Photo
Importance of Fluvial SystemsEnvironmental issues:
floodingwater transportagriculturesoil erosionnutrient transport
Importance of Fluvial SystemsResource issues-Facies models for hydrocarbon plays and groundwater reservoirs-Sensitivity to changes in climate and tectonics
Channeled Scablands WA Megaflood Bedforms
Fluvial Channels as Hydrocarbon Reservoirs Sands
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Subenvironments in Fluvial Systems
Channels LeveesFloodplainsLakesSwamps
Classification of Fluvial SystemsClassification-based on shape # and stability of channelsSinuosity index (S) = Lthalweg (deepest part of channel) / Lvalley
l. MacKenzie River Canada), Utrecht U. r. Columbia R., CA H Berendsen Photo
Classification of Fluvial Systems
Braided-multiple, shallow, unstable channels-for a given discharge higher slopes than meandering streams-mid channel bars-floodplains and levees less important
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Why one type of river vs. another?Controlling Variables for Fluvial Systems
Flow Characteristics:(Controlling variables: amplitude, periodicity, amount of change)
Discharge
Slop
e
Independent variables:•Slope (tectonic controls)
•Discharge/variability (climatic control)•Sediment load (amount and particle size)
•Bed roughness
Graph data from Smith 1993
Meandering Stream Facies ModelMost typical of humid regions
zones of more constant discharge, moderate slope conditions)
Channel morphology and channel floor deposits thalweg, x-sectional asymmetry, cut banks,cross-overs, marginal point bars)
Meandering Stream Facies Helical FlowDownstream transport-superelevation of water surface on outside bends (nb typo)-pressure differential causes secondary helical flow
Lateral Accretion
Erosion
Meandering Stream Facies Helical Flow
Particle size fining up point bar with reduced shear stress
Lateral Accretion
Erosion...
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Point Bar- Fining Upwards SequencesFrom channel bottom upwards:1-Basal erosion
Tabular sands encased in mud rocks (muds predominate)-Epsilon x-beds & fining up sequences characteristic of sands-Abundant and extensive paleosols
Stratigraphic Geometry of Meandering Stream Deposits
Chinle Fm (Petrified Forest) Morrison Fm. CO
P. Heller photo
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Anastomosing Rivers-FormationForm where abundant accomodation space exists for vertical aggradation of channel and bed. Low slope conditions-e.g.: behind dams, during rapid subsidence, rising base level.
Saskatchewan R. N. Smith photo
Anastomosing River ChannelsChannels: Multiple, often (but not always) low sinuosity channels-stable position-Dynamics characterized by avulsion rather than migration-Gravels, trough and planar x-bedded sands, ripple x-laminated sands
Overbank deposits-massive or mottled silts, micritic ls., coalsL. Cosumnes R. (U.C. Davis photo). R. Upper Columbia R. (H. Berendsen photo)
Photo
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Anastomosing River Deposit GeometryIsolated shoestring sand channels from avulsion(100-1000m wide, 10s of m thick, 10s of km long) Encased in mudrocks (overbank, wetland deposits)Fossils-coals/plant fossils in overbank
Channel SandsSt, Sp, Sh
Shoestring SandPaleochannel
LeveeSr, Fsm
Crevasse SplaySr, Sp, Sm
Wetlands, OverbankFm, Fcm
Bioturbated, paleosols
Braided Rivers
Form under conditions of high, mobile sediment supply and high slope-Characterized by multiple, mid channel bars (large scale bedforms). -On scale of channel depth these are large features-Multiple unstable, shallow channels-low sinuosity
Braided River BarsActive during floods of entire channel beltSize- 100s-1000s m long, 10s-100s m wide, few-15m high
Photo
Longitudinal BarsTear drop shaped, elongate downstream pointing downstream,
-typical of channel center in gravelly streams -fine downstream so coarsen upsection as bar migrates-often imbricated)
Toutle R., longitudinal bars. Flow to right.
P. Heller photo
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Transverse BarsLook like large ripples
-typical of sandy systems-often well developed slipface-often assoc. w/ 3-D ripples climbing bar and in channel