Ch. 16 Flashcards
(25 cards)
stream
any channeled flow of water
fluvial process
those that involve running water, encompass both the unchanneled downslope movement of water called overland flow. and the channeled movement of water along the valley bottom called stream flow
valley
portion of the terrain on which a drainage system is clearly established
interfluve
the higher land above the valley walls that separate adjacent valleys
drainage basin or water shed
all the area that contributes overlain flow, stream flow, and groundwater to the stream
fluvial erosion and deposition
remove sediments and transport them to another location, the movement and deposition by water creates very different landforms
erosion by overland flow
fluvial erosion begins when rain starts to fall. infiltrates soil,
erosion by stream flow
erodes and transports materials. volume and velocity of water has a significant effect
transportation
movement of rock material
stream load
material that reaches stream and is then carried. three component
dissolved load
minerals that are dissolved in the water and carried in the solution
suspended load
very low settling sped, particles of clay and silt. carried along in the water without ever touching the stream bed
bedload
sand gravel and larger rocks fragments, jumps or bounces along with stream or the larger pieces are rolled
deposition
whatever has been carried by the stream is eventually set down.
alluvium
stream deposited sediment.
stream channel patterns
straight-short, sinous-irrgular and gentle curvature, meandering-highly variable, braided-multiple interwoven channels
dendritic drainage pattern
treelike and branching, most common
trellis pattern
alternating bands of tilted hard and soft strata (bedrock), with long parallel streams linked by short rigid angle segments. ridge and valley areas
radial pattern
develop around an elevated central point such as a volcano
deranged
develop from an interruption of a pre existing drainage pattern
floodplain
wide low lying areas around a river
levees
low banks that suffice to keep the stream in its channels during normal flow
bluff/escarpment
steep slopes at the outer edge of the floodplain
alluvial fan
fan shaped landform that develops when a high velocity stream carries large bed loads and discharges the load into a broad flat valley floor