River Series 3 Flashcards
In topographically low parts of the landscape ______, ________, and _________ sediments are deposited
valleys, pidemonts, coastal plains
Fluvial sediments are laid down, and depositional landforms are created at:
- Dominantly or partially subaerial conditions
- Topographic discontinuities
- Valleys and the margin of water bodies
Restricted lateral movement and confined within the valley
upstream channel
Channels are able to shift positions over wide areas
Near baselevel
Arid to Semi-Arid Environments
Large Sediment Supply
Occurs in Fault fronts, Tectonic Mountain Fronts or Sudden Topographic Discontinuities
General gradient: 3-6°
Marginal screes: ~30°
Near the apex: ~10°
Alluvial Fans
Upper part is incised passing outward to braided streams. Generally poorly sorted sediments near the head due to torrential deposition. It becomes better sorted sediments outwards with finer grains
Fan structure
Conglomerates/unsorted sediments near the head, with bettering sorting and finer-ing of sediments outwards.
Sediment mechanics of alluvial fans
Exhibits complex cross-bedding and Flow Structures
Bedding
an size should be related to the size of the sediment source area AKA drainage basin.
Growth of fans
Have a smaller fan, compared to fans underlain by mudstone and shale
Geology influences the relation, in a drainage basin e.g underlain by sandstone
Fan surface is not dissected. Relatively smaller than fans of perennial streams
Dry fans
Streams flows through incision. Coarser materials are rarely carried downstream. River widens downstream, braided. Progressively shifting channel
Wet fans
Where alluvial fans are large enough, or sufficiently closely spaced, they may coalesce laterally to produce a depositional bed. To produce a __________.
Peidmont zone or Bajada
Mainly are terraces and floodplains of a river. Normally finer upward. Channels are mainly braided to meandering though some other rivers
Valley fills
Change in positive baselevel change: resulting into the backfilling of the
Uplift or Change in climate: resulting into increased sedimentation, sediment load progressively moves down the system
Uniform filling of the valley: increase in production of sediments from the numerous tributaries
Valley Filling
Enumerate the channel types in valley fills
Meandering
Anastomosing
Braided
Straight
Sinuous Channels
Near Baselevel
Low Gradient/Flat
Fine Sediments (Mainly suspended loads and dissolved loads)
Shifts laterally
Meandering channels
Low Bedload discharge
Low sinuousity
Low bedload unless due to incision
Straight
Relatively permanent
Cohesive banks, Sinuous channels
Diverges/Converges around stable, vegetated bars
Anastomosing stream
High sediment supply
High Gradient changes
Low stability
Braided
Enumerate the causes of braiding
Overloading of sediments discharge
Steep slopes which produce a wide shallow channel where bars and islands form readily
Easily erodible banks which permit widening at high flow
Large bed material load, in comparison with its suspended load where large material is immobile except during high flood stages
Alluvial surface adjacent to a channel that is frequently inundated. Highest elevations normally occurs on the abandoned levee and point bar ridges
Floodplains
Occasionally be formed by the incision of bedrock surfaces, but they are most likely the remnants of floodplains trenched by rivers. Caused by negative baselevel changes- resulting into headward surges of rejuvination
River terraces
______ may represent reworking and may contain heavy mineral concentrations
Terrace sediments