Erosion and Running Water
Steven Dutch, Natural and Applied Sciences, University
of Wisconsin - Green Bay
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- The vertical drop of a stream in a given horizontal distance is its:
- discharge
- base level
- gradient
- drainage pattern
- velocity
- The _____ drainage pattern resembles the branching of a tree.
- rectangular
- deranged
- trellis
- radial
- dendritic
- Sediment transport by intermittent bouncing and skipping along a stream bed is:
- saltation
- suspended load
- dissolved load
- alluvium
- capacity
- Trellis drainage is most likely to develop on:
- natural levees
- tilted sedimentary rock layers
- granite
- horizontal layers of volcanic rocks
- fractured basalt
- Ridges of sediment deposited on the margin of a stream are called:
- natural levees
- incised meanders
- oxbow lakes
- alluvial fans
- bottomset beds
- The direct impact of running water is called:
- bed load
- meander cutoff
- saltation
- base level
- hydraulic action
- The capacity of a stream is a measure of its:
- volume of water
- discharge
- velocity
- ability to erode
- total load of sediment
- A meandering stream is one having:
- numerous sand and gravel bars in its channel
-
a single, sinuous channel
- a broad shallow channel
- a deep, narrow valley
- long, straight reaches and waterfalls
- In which of the following do foreset beds occur?
- alluvial fans
- deltas
- point bars
- natural levees
- deltas
- Which of the following controls flow velocity in streams?
- channel shape
- gradient
- depth
- channel roughness
- all of these
- The feature separating one drainage basin from another is a(an):
- divide
- valley
- natural levee
- point bar
- alluvial fan
- A drainage pattern in which streams flow in and out of lakes with irregular flow directions is:
- radial
- rectangular
- longitudinal
- graded
- deranged
- The primary process by which bed load is transported is:
- suspension
- precipitation
- abrasion
- answers (a) and (c)
- saltation
- Which of the following is a local base level?
- lake
- point bar
- ocean
- alluvial fan
- floodplain
- Erosional remnants of floodplains that are higher than the current level of a stream are:
- oxbow lakes
- incised meanders
- cut banks
- natural bridges
- stream terraces
- All of the sediment carried by saltation and rolling and sliding along a stream bed is the:
- suspended load
- bed load
- drainage capacity
- channel pattern
- stream profile
- The dry lake beds in many deserts are:
- playas
- pediments
- bajadas
- mesas
- inselbergs
- A stream can lengthen its channel by:
- runoff
- hydraulic action
- headward erosion
- downcutting
- vertical accretion
- The removal of thin layers of soil by water over a more or less continuous surface is
- gullying
- leaching
- sheet erosion
- exfoliation
- weathering
- Why are the Rockies high?
- They get little rain and are not eroded.
- They are still young and have not been eroded away.
- They are not subject to chemical weathering.
- They get little acid rain.
- A dam will most likely:
- accelerate erosion upstream
- not affect the river downstream
- cause the reservoirs to fill with sediment eventually
- accelerate erosion above the reservoir
- All of these can result in a canyon cutting through a ridge. Which one is
least likely to be the correct explanation?
- the crust is uplifted
across the course of the stream
- the stream erodes down into
a buried ridge and the overlying cover is stripped away
- a huge flood carves a
canyon
- a peneplain is uplifted and
resistant rocks form ridges
- In uniform flat rocks, drainage patterns tend to be
- dendritic
- radial
- trellis
- braided
- Which factor does not directly influence the shape of a delta?
- intensity of wave action on the shore
- strength and height of tides
- width of the continental shelf
- volume of sediment carried by the river
- none of the above
- The principal reason rivers do not fit the idealized erosion cycles of youth-maturity-old age:
- they flow across rocks of varying hardness
- climate is not constant over large river basins
- global sea levels have changed markedly in the last few thousand years
- The process by which one stream loses a major portion of its headwaters to another stream is called:
- stream larceny
- stream theft
- stream piracy
- perifluvial capture
- none of these
- River channels which were abandoned by a captured stream are now sometimes seen as:
- water gaps
- hanging valleys
- nick points
- wind gaps
- none of these
- An old-age stream
- is at least 10,000 years old
- is at least 1,000,000 years old
- has a straight course with few bends
- is of no definite age but flows across a low landscape and has many meanders
- A stream that has more sediment to move than it can carry at one time is likely to be
- mature
- meandering
- braided
- youthful
- How levees form along rivers
- built by Army Corps of Engineers
- built up by deposits laid down when the stream floods
- form when clay along the river bank dries out and swells up
- are piled up by aquatic organisms
- The gently sloping rock surface that forms at the base of mountains in arid regions
- playa
- graben
- pediment
- stratum
- Landscapes can be rejuvenated
- at any time
- any time except old age
- only during maturity
- only during old age
- These are all names for hills or mountains that form when erosion leaves remnants behind, except one. Which is not?
- plateau
- mesa
- inselberg
- monadnock
- Not a major factor in arid erosion
- lack of vegetation
- intense chemical weathering
- thin soil cover
- episodic rainfall
- This kind of drainage suggests stream piracy
- dendritic
- barbed
- braided
- trellis
- This kind of drainage suggests strong variations in erosional resistance of
the bedrock:
- dendritic
- meandering
- trellis
- deranged
- You see a stream cutting right through a ridge. This landscape is called:
- old-age landscape
- rift valley
- antecedent or superposed
drainage
- rejuvenated landscape
- peneplain
- A stream cutting right through a ridge implies:
- the ridge was split open by
some kind of upheaval
- a huge flood carved a
canyon through the ridge
- the stream predates the
ridge
- the landscape is very
young
- the rocks in the ridge are
highly weathered
- Why do rivers meander?
- The land is flat
- The landscape is millions of years old
- The river suddenly slows down
- The river suddenly speeds up
- The gradient of the river increases
- When two third-order streams join, the result is a _________ order stream
- First
- Second
- Third
- Fourth
- Fifth
- River deltas on coastlines where wave action is important tend to
- Build far offshore
- Be spread along the coastline
- Have many parallel islands and channels
- Have a smoothly curved front
- River deltas on coastlines where tides are dominant tend to
- Build far offshore
- Be spread along the coastline
- Have many parallel islands and channels
- Have a smoothly curved front
- River deltas on coastlines where deposition is most important tend to
- Build far offshore
- Be spread along the coastline
- Have many parallel islands and channels
- Have a smoothly curved front
- River deltas on coastlines where wave action and deposition are about equally important tend to
- Build far offshore
- Be spread along the coastline
- Have many parallel islands and channels
- Have a smoothly curved front
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Page Created 31 December 1996, Last Update
13 December 2004