Unit 4.5: External forces fluvial Flashcards
what is a drainage basin?
an area of land that is drained by a single stream and its tributaries.
what characteristics/features does a drainage basin have?
- trunk stream: single large stream into which smaller streams merge
- tributary: stream that joins with other streams to form a single stream
- mouth: end of stream where it meets a larger body of water
what are drainage divides?
drainage basins are separated by these ridges or highlands but the water ends up in the same place
what are continental divides?
ridges or highlands that separate drainage systems that empty into different ocean basins
what are drainage patterns?
arrangements of channels in an area; determined by regional steepness, rock resistance, climate, and hydrology
what are some various types of drainage patterns?
- dendritic: they’re little tributaries that look like tree branches and slope gently in the direction of the stream
- deranged: no clear geometry; develops in areas having disrupted surface patterns. its almost like different lakes that are all connected.
- radical: drainage of a conical mountain flowing in all directions
- rectangular: right-angle contacts between streams and tributaries. formed by faulted and jointed landscapes
- trellis: streams flow in only two orientations; developed on parallel folded or dipping rocks
- centripetal: centric pattern, stream segments drain the interior of an excavated dome.
what are stream orders?
the ranking of streams in a drainage basin based on signs.
- 1st order: smallest streams with no tributaries
- 2nd order: when two or more streams join (has tributaries)
what is stream permanence?
indicates how permanent a stream is
what are the different types of stream permanence?
- intermittent stream: run dry for part/most of the year
- ephemeral stream: flows briefly only after heavy rain
- permanent stream: flows year round
- exotic stream: permanent stream that originates in humid region and flows through arid regions (like the nil)
what is fluvial erosion?
erosion by running water
what influences the rate of erosion for a stream?
- lithology: rock type underlying the stream
- stream discharge: the faster stream = more erosion
- location of stream: steep gradient, small channel, greater erosion means more erosion
what are some different types of erosion?
- Abrasion: mechanical action; the movement of one material wears away at another material
- Hydraulic action: water dislodges and drags away rock material from bed and bank. like plucking
- solution: dissolving of rock material by water
define “stream load”
material that moves in a stream channel
what are the 3 types of stream load?
- dissolved load: material that is invisible dissolved particles. its main contributor is chemical weathering.
- Suspended load: fine sediment, largest type of stream load. turbulence is key to holding it in suspension.
- bed load: material that is bounded (saltation) or rolled (traction) along stream bed; heavier particles
what are antecedent streams?
cut through bed rock ridges rather than flow around them
what are superimposed streams?
cut through resistant layers of rock and form water gaps
what is stream sorting?
as velocity decreases, sediment will be deposited and sorted by size. heaviest would drop first
what is an alluvial fan?
created by stream sorting gently sloping accumulation of sediment deposited at the base of a mountain or arid environment.
Define “stream gradient”
steepness of a stream, more gradient means more steep
what is a braided stream?
channel breaks into many tributaries that diverge around sand and gravel bars and then converge again.
what are meandering streams?
channels that are sinus in form and weave across landscapes. sinuosity is the ratio of actual distance to straight line distance.
what is aggradation?
build up of sediments in a stream and floodplain.
when do meandering streams occur?
when suspended load is greater than bed load and presence of random obstacles cause sinuosity.
what features are related to a meandering stream?
- Thalweg: fastest flowing water in the stream. this is what erodes the bank to form the bend.
- point bar: the opposite side that does not get eroded, water is slower
- cutback: the part that gets eroded and forms the meander.
- meander neck: distance between bends in meanders that are next to each other
- oxbow lake: an isolated meander fromed where there is a cutoff; may fill with sediment over time.
what are other features that are common in fluvial dispositional environments?
- floodplain: flat, low-lying ground on either side of the stream channel
- yahoo stream: tributary that is prevented from joining the main stream; flows parallel to main stream
- wetlands: permanently flooded area
- natural levees: broad ridges that run along both sides off the channel. built up by recurrent floods (made by alluvium)
- delta: fan shaped accumulation of sediment that forms where a stream meets with a larger body of water. when the water from the stream enters the larger body, the velocity reduces and the sediment is immediately deposited.