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buttsuni buttsuni
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Posts: 515
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6 years ago
Using Figure 16.17, list the stream properties that increase with downstream distance and those that decrease.
 
  Then, explain which properties are most responsible for the increase in sediment load with downstream distance and the decrease in the grain size of the sediment load with downstream distance.
  What will be an ideal response?



Q. 2 - Describe the processes that naturally form lakes.
 
  What will be an ideal response?



Q. 3 - What is the difference between stream discharge and stream velocity? What are the units used to measure discharge and velocity? Why does stream discharge change along the length of the stream? Why does stream velocity change along the length of a stream?
 
  What will be an ideal response?



Q. 4 - What would you suspect to be the cause of dramatic differences in the sediment load per square kilometer between two streams with very similar climates?
 
  What would you suspect to be the cause of dramatic differences in the dissolved load per square kilometer between two streams with very similar climates?
  What will be an ideal response?



Q. 5 - Consider a planet with little precipitation. What would the landscape look like compared to Earth?
 
  What will be an ideal response?



Q. 6 - What is the difference between the saturated zone and the unsaturated zone? What is the name of the undulating surface that forms the top of the saturated zone?
 
  What will be an ideal response?



Q. 7 - List the positive and negative consequences of building a dam on a river.
 
  What will be an ideal response?
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Replies
wrote...
6 years ago
(Answer to question 1 )  Stream Properties That Increase with Downstream Distance
Discharge
Sediment load
Channel width
Channel depth
Flow velocity

Stream Properties That Decrease with Downstream Distance
Grain size of bedload
Elevation of channel bed
Slope of channel bed
Stream power
Shear stress

(Answer to question 2 )  Lakes form naturally where lava flows and mass-movement deposits block a stream channel or where faults shift crustal blocks downward to produce a central depression that collects water.

(Answer to question 3 )  A stream's discharge is the volume of water passing a given point for a specific amount of time. The stream's velocity is the speed of the water. The units for discharge are cubic meters per second (or cubic feet per second) and the units for velocity are meters per second (or feet per second).

(Answer to question 4 )  If two streams have very similar climates but very different sediment loads per given area, I would suspect that they have a dramatic difference in relief. The stream with the high sediment load would have steep relief.
If two streams have very similar climates but very different dissolved loads per given area, I would suspect that they have a dramatic difference in rock type. The stream with the high dissolved load would have an abundance of soluble rocks like limestone. The stream with the low dissolved load would have an abundance of less soluble rocks like granite.

(Answer to question 5 )  Sediment production would dominantly be mechanical, with little sediment produced. The sediments produced would remain in place or be transported by winds.

(Answer to question 6 )  The saturated zone is the portion of rock or regolith where the pores are completely filled with ground water. In the unsaturated zone the pores are filled with air and ground water. The top of the saturated zone is called the water table.

(Answer to question 7 )  Positive
Control floods by impounding high discharges
Provides water during the dry season
Generation of electricity
Negative
Dams fill up with sediment
Enhanced erosion downstream of a dam
Changes in channel size and shape downstream of a dam
buttsuni Author
wrote...
6 years ago
Passed my quiz with this!
wrote...
6 years ago
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