Chapter 16 Flashcards
Overland flow
unchanneled downslope movement of water
Streamflow
chaneled movement of water
valleys
portion of terrain in which a drainage system is established
interfluve
higher land above valley walls that separates adjacent valleys
drainage basins
areas that drain to the valley; watersheds; drainage divide
stream order
smaller streams join larger ones; smaller numbers are more frequent; larger numbers are longer streams
Stream competence and capacity
stream competence: measures maximum particle size a stream can transport
stream capacity: measures the amount of solid material a stream can transport
erosion by streamflow
once channeled, erosion is enhanced; erosion increased by debris; streamflow picks up; chemical weathering—corrosion
straight channels
short and indicative of strong geologic structure control
sinuous channels
irregular and gentle curvature
meandering channels
highly variable curvature
braided streams
multiple interwoven channels separated by loose bars or islands
dendric pattern
treelike pattern with random merging of streams
trellis pattern
forms in areas of hard and soft bedrock in close content; shape modified by structure of bedrock
radial pattern
streams descend in a concentric uplift (like a volcano)
centripetal pattern
streams converge into a uniform basin (like a 2D funnel)
valley deepening–downcutting
hydraulic power of moving water to lower the streambed
valley deepening–base level
lower limit to the amount of downcutting can occur–base level is sea level
valley deepening–knickpoints
channel irregularities such as rapids and waterfalls
valley widening
widening slows above base level; as gradient decreases, stream flow meanders and lateral erosion occurs; fastest on outside of curves (cut bank); slowest water on inside of curve accumulates alluvium (point bar)
floodplains
humans live on these; flat land, abundant water, productive soil
delta formation
slowed flow when it reaches an ocean or lake results in deposited sediment; this debris builds up and forms a delta
deposition valleys cause
aggradation
evolution of a cutoff meander
erosion, cutoff meander, oxbow lake, meander scar