4.6 Flashcards
What is meant by the long profile of the river?
It shows you how the gradient (steepness) changes over the different courses
How does the river Eden’s landscape change along its long profile
(upper/middle/lower). Consider: channel shape, valley profile, gradient,
discharge, velocity and sediment size and shape?
Upper: v- shaped, discharge is low, narrow channel, low channel depth, low velocity, lots of sediment load size, high slope angle gradient
Middle: u-shaped, discharge is medium, wider channel, mid channel depth, higher velocity, less sediment load size, lower slope angle gradient
Lower: wide flood plain, high discharge, wide channel, deep channel, high velocity, barely any sediment size, low slope angle gradient.
What are the reasons for river discharge changing as it goes downstream
More tributaries have joined, drained a much larger part of the drainage basin
What are the reasons for channel width changing as it goes downstream
More discharge, tributaries have joined, velocity got quicker, more erosion power, lateral erosion
What are the reasons for channel depth changing as it goes downstream
More discharge, vertical erosion, more tributaries in it, higher velocity
What are the reasons for velocity changing as it goes downstream
Shape is wider and deeper, its bed and banks are smoother
What are the reasons for sediment load size changing as it goes downstream
River is flowing at higher velocity, therefore higher rate of abrasion, angular beds and banks upstream too
What are the reasons for slope angle (gradient) changing as it goes downstream
Upper course traction transport erodes downwards and creates vertical erosion. In lower course suspension transport is laterally eroding
Compare hydraulic action with abrasion
HA : water hits banks
A : MATERIAL rubs against banks
Define weathering
Weathering is the breakdown of rocks at the Earth’s surface, by the action of rainwater, extremes of temperature, and biological activity. It does not involve the removal of rock material. There are three types of weathering, physical, chemical and biological.
Compare freeze thaw and biological weathering
FT: happens inside the water
BW: happens in cliff cracks but they both happen in cracks in the rock
Compare traction with suspension transport
T: stones roll along bed, large sediment
S: the water flow carries silt and small particles
Different sediment sizes
Explain the stages and processes responsible for waterfall formation
More resistant rock lies over less resistant rock
Less resistant rock erodes more easy by abrasion and hydraulic action.
At the foot of waterfall water swirls and erodes the bed making a plunge pool
Once resistant rock has eroded the more resistant rock collapses and this process happens lots until a gorge is formed
Compare a flashy and subdued hydrograph
Flashy: high peak discharge and rainfall
Subdued: low peak discharge and rainfall
Explain the stages and processes responsible for v shaped valleys and interlocking spurs
River erodes down due to gravity, less energy so no lateral erosion
Weathering occurs on the valley sides
Slope transports transports sediment off the sides to the rivers
V shaped valley is left
River weaves around bands of more resistant rocks as river is not able to erode hard rocks