rivers and floods Flashcards
What is base level?
- deepest level to which streams can erode
- usually sea level (but not always)
- determined often by global sea level
- water must follow gravity
- ex. a dam can change local base level
what is a stream and what determines the size
- a body of water confined within a channel, supplied with water by its drainage basin
- interchangable with river/creek
- it doesnt matter how large or small it is
size determinants:
- climate
- size of drainage basin
- substrate
- vegetation
stream valley
SEE NOTES
- area between tops of slopes on both sides of the river
channel
SEE NOTES
- trough through which water flows
flood plain
- area that will flood in times of increases precipitation
SEE NOTES
thalweg
line connecting deepest parts of the channel
discharge
- volume of water flowing downstream/unit time (m^3/sec)
where are highest flow veolcities in a stream
straight areas
- centre of channel
- just below water surface
around meanders
- outsider of meander bend
- friction from channel itself and air friction causes this
how does the shape of a valley change downstream
cross sectional profiles
- steep-sided, v-shaped near source, canyons
- broader valleys donstream
- the valley changes shape
- the volume of water increases the farther down it goes so there is increased erosion
how does the slope of a stream change downstream
longitudinal profile
- steep gradients near source
- low gradients downstream (angle of elevation
what kinds of forms can streams have?
- meanding streams
- obow lake
- floodplain
- braided stream
channel morphology
- sinuosity is used to classify channels
- ratio of stream length: valley length
- low sinuosity is not very bendy and high sinuosity is bendy
- there is straight and meandering streams
- sinuosty is calculated by the stream and valley length
meandering streams
- common in areas with low slopes
- thalweg close to outer bend of meander
- most erosion occurs at the outside bend of meander- deepest water, highest flow velocityes- cutbank
- most deposition- inside bend of meander- point bar
- ex. innoko national wildlife refuge, alaska
erosion of cutbank, deposition of point bar= migration of meanders - meaders can join and form neck cut off since the water will go through point of least resisitance
- on th point bar:deposits sands and silts (ripples and dunes)
- on floodplain: deposites silts and clays (because its not moving)
- with migration forms: fining upwards sequence
oxbow lake
- crescent shaped laked formed where a meander is cut off from a stream
- ex. slave river, northwest territories
floodplain
- broad strip of land built by sedimentation on each side of the channel
- covered when river floods (floods during increased precipiption)
- coasrest material depositied closest to the channel- formed LEVEES (these are not strong and wont protect againt future floods)
- finer grained material carried futher away- clays and silts
- is is bas idea to build on a flood plain