Rivers Flashcards
what is river planform
the configuration of the channel in a plan view or aerial
what is an alluvial river
a river that flows through the sediments or alluvium
what is a reach
a length of river that has uniform appearance in both character and behaviour.
what is a segment
an alternating sequence of reaches
what is a geomorphic unit
a discrete channel or floodplain unit
what is lateral accretion
coarse sediment deposited inside a meander bend which gets incorporated into the floodplain.
what is vertical accretion
the vertical rise of a floodplain due to the overbank deposition of suspended load.
what are levees
a ridge along the channel with suspended and bedload couplets due to overbank vertical accretion
what is a backswamp
the lowest part of the distal floodplain which has fine grained sediments
what is a crevasse splay
when the levee breaches depositing bed load.
what is a cutoff
when a meander bend cuts through its neck leaving a paleochannel
what is the energy, sediment mix and valley setting of high energy floodplains
- > 300 W/m2
- non cohesive sands and gravels with some boulders
- confined and partly confined valleys on high slopes
what is the landscape position, formation and reworking processes and river type of high energy floodplains:
- uplands and headwaters
- vertical and abandoned channel accretion
- floodplain stripping, channel widening and floodchannels
- confined valley and partly confined
what sculpted features are found with high energy, high slope
waterfalls, step pool, cascades, rapids, riffles and runs
what mid channel depositional units are found
boulder mound, longitidunal bar, diagonal bar, transverse bar, islands and gravel/sand sheets
what bank attached features can be found
lateral bars, point bars, ledges, tributary confluence bars and benches
what sculpted fine grained erosional features can be found
sculpted point bars, sculpted lateral bars, runs and poolsha
what are the two mechanisms of accretion that build floodplains
lateral and vertical accretion
what is the energy setting, sediment mix, valley setting and landscape position of medium energy floodplains
10-300 W/m2, non cohesive sands and gravels, partly confined and middle to lower reaches
what is the formation and reworking processes and river types of medium energy floodplains
vertical and or lateral accretion
avulsion, cut offs, channel expansion and floodchannels
braided, meandering and wandering gravel bed
what is the energy setting, sediment mix, valley setting and landscape position of low energy floodplains
<10 W/m2
cohesive sands, silts and clays
wide, alluvial valleys on low slopes
lower valley reaches
what is the formation and reworking processes and river types of low energy floodplains
vertical accretion
abandoned channel and avulsion
anastomosing, discontinuous watercoarses
what are flood channels
a channel cut through the floodplain initiated upstream by flows shortcutting the floodplain pocket
what are cut offs
a shortening of the channel by cutting through the neck of a meander bend
what is avulsion
occurs when a river is ready to shift channel state. a decrease in channel stability over time may lead to a breach of avulsion threshold.
what are the 3 process zones in a catchment
source, transfer and accumulation
what does a squashed hydrograph mean
long distances between tributaries, not geomorpically significant and dont experience flash floods as often
what does a peaked hydrograph mean
short distance between tributaries, geomorphically significant and experiences flash floods.
how to calculate relief ratio
maximum relief / basin length
why are most rivers show a concave longitudinal profile
because they are trying to erode to base level
what makes longitudinal profiles irregular
geological and long term environmental changes
what is sediment limited transport
when a river doesnt have enough sediment to transport due to higher carrying capacity. these rivers will be erosional and incise (headwaters region)
what is transport limited transport
when a river cant move the sediment. sediment is too large (competence limited). the sediment supply exceeds the capacity of transport (capacity limited)
what happens along the drainage area of a catchment
bedload size decreases, stored alluvium increases and width, depth, flow velocity and discharge increases
what are the 5 scalar components of a river landscape
catchment
landscape unit - valley setting
reaches - gorge river, meandering stream
geomorphic units - benches, cutoffs
hydraulic unit - water characteristics such as turbulent flow
formula for total stream power
() = yQs
y =specific weight of water
Q = discharge
s = slope
what are imposed boundary conditions
they do not adjust over geomorphic time, produce the valley setting for a river (confined or unconfined) and contain the base level of the river
what are flux boundary conditions
dynamic with sediment and flow regimes. (EDIT)
a river with single channel, <1.5 sinuosity, reflect imposed boundary conditions and laterally stable
straight rivers
a laterally unstable, with multiple thalwegs, indicative of high and low flow conditions, sinuosity <1.5 and where flow diverges and rejoins multiple times
braided river (tasman river)
absent or discontinuous channels, laterally unstable and prone to channel infilling and incision
discontinuous coarse rivers (down south near bega)
usually single channel, high sinuosity and laterally variable. contains mixed or suspended load
meandering river (colo river)
up to 3 channels, bedload dominated, water flows around islands or vegetated bars
wandering gravel bed rivers (rivers in NZ)
a multi channeled, low sinuous river with laterally stable channels that are prone to avulsion. the channels are separated by floodplains
anastomosing rivers (outback aus)
what valley setting has discontinuous floodplains
partly confined
what valley setting has isolated or absent floodplains
confined