According to Fenneman’s postulation, why is there least effective rainwash at the hill-top?
Options:
Due to under-loaded surface runoff
Due to less volume and velocity of surface runoff
Due to the presence of debris carried by surface runoff
None of the above
Option: B
According to Lawson’s postulation, why does erosion by surface runoff at and near hill-tops become most active?
Options:
Because surface runoff carries more debris
Because surface runoff carries less debris
Because the slope angle is steeper at the hill-top
None of the above
Option: B
According to Lawson’s theory, what are the two distinct zones in hillslope profile?
Options:
Zone of erosion and zone of deposition
Zone of erosion and zone of aggradation
Zone of weathering and zone of erosion
None of the above
Option: B
What happens to the radius of the curvature of longitudinal profile of hillslope with time, according to Lawson’s theory?
Options:
It decreases
It remains constant
It increases
None of the above
Option: C
Why does erosion energy of surface runoff decrease downslope, according to Lawson’s theory?
Options:
Due to increased volume of runoff
Due to decreased velocity of runoff
Due to the presence of more debris downslope
None of the above
Option: C
What is responsible for the development of basal concavity in hillslope?
Options:
Deposition of debris
Active erosion mainly by rill and gully erosion at the slope base
Soil creep and rainwash
Local conditions determine if it is depositional or erosional
Option: B
What is the poly-process concept of slope development?
Options:
Only one denudational process operates on a slope profile
Different denudational processes operate together on a slope profile
Denudational processes operate in opposite directions on a slope profile
There is no relation between slope profile and denudational processes
Option: B
Which denudational processes are recognized as the most active slope forming processes?
Options:
Deposition of debris
Soil creep and rainwash
Fluvial erosion
None of the above
Option: B
What is responsible for the development of summital convexity in humid temperate regions?
Options:
Soil creep
Rainwash
Fluvial erosion
Deposition of debris
Option: A
What is the relationship between soil creep and rainwash in the development of hillslope?
Options:
Soil creep and rainwash operate independently on different segments of the hillslope
Soil creep and rainwash are agents of transportation of debris
Soil creep and rainwash are not slope forming processes
Soil creep and rainwash operate together on hillslope
Option: A
What is the process of slope decline in the Davisian model of slope evolution?
Options:
There is progressive increase in slope angle from youth to old stages.
There is no change in slope angle but the slope form changes from youth to old stages.
There is progressive decline in slope angle and sequential change in slope form from youth to old stages.
There is no change in slope angle or slope form from youth to old stages.
Option: C
What is the cause of slope decline in the Davisian model of slope evolution?
Options:
Active downcutting and valley deepening during the youth stage.
Continued lateral erosion and downwasting of water divides during the mature and old stages.
Soil creep and alternate dilation and contraction of soil under the influence of gravity during all stages.
Weathering and erosion by wind and water during all stages.
Option: B
What is the difference between slope replacement and parallel retreat in terms of the maximum angle and concavity of the slope?
Options:
In slope replacement, the maximum angle decreases and the concavity becomes segmented, while in parallel retreat, the maximum angle remains constant and the concavity increases in length.
In slope replacement, the maximum angle remains constant and the concavity becomes smoothly curved, while in parallel retreat, the maximum angle decreases and the concavity becomes segmente
In slope replacement, the maximum angle decreases and the concavity becomes smoothly curved, while in parallel retreat, the maximum angle remains constant and the concavity increases in length.
There is no difference between slope replacement and parallel retreat in terms of the maximum angle and concavity of the slope.
Option: C
What is a graded waste sheet?
Options:
A layer of waste material on a slope
A type of weathered rock
A type of soil erosion
A type of rock formation
Option: A
When does the condition of graded waste sheet begin?
Options:
From the top of the slope
From the middle of the slope
From the base of the slope
From the summit of the slope
Option: C
At what point does a graded slope lead waste down to the streams?
Options:
At any point
Only from the top of the slope
Only from the middle of the slope
Only from the base of the slope
Option: A
How does the gradient of a valley side slope change as the cycle of erosion advances?
Options:
It becomes steeper
It becomes more gentle
It remains the same
It is unpredictable
Option: B
What dominates the upper part of the valley side slopes?
Options:
Basal convexity
Summital concavity
Basal concavity
Summital convexity
Option: D
What does the increase in length of convex and concave segments signify in slope profile evolution according to Davis’ model?
Options:
A flattening of slope profile
An increase in slope angle
A decrease in slope angle
A steepening of slope profile
Option: A
What is the main factor on which the Davisian model of slope evolution depends?