L3 - Changing Course Flashcards
How long is the River Severn and where is it geographically located?
UK’s longest river at 354km
Rises in mid-Wales, flows east into England and then south into the Bristol channel
How does the gradient develop with the River Severn?
Upper course - steep, V-shaped valleys and interlocking spurs present
Middle course- flatter, still fairly steep, meanders and ox-bow lakes form
Lower course - flat, deltas, levees, flood plains
What is discharge?
The volume of water that passes through a cross-section per unit time
Measured in cumecs (cubic metres per second)
Increases the further downstream
Describe features of the upper course in the River Severn.
Geology - hard rock (impermeable shale and grit)
Near the river source (Plynlimon 610m above sea level) - narrow and shallow channel, angular stones slowing river down due to friction
Describe features of the middle course in the River Severn.
Softer, permeable rock - sandstone
Wider and deeper due to erosion, velocity increases
Describe features of the lower course in the River Severn.
Geology - mudstone, sand, gravel
- River channel widens, discharge increases
What happens to discharge downstream?
Increases
More tributaries join the river draining a larger catchment area increasing the volume of water.
- Channel width is greater due to erosion further up the course, gradient decreases and width increases faster than depth.
What happens to river velocity downstream?
Increases
River is smoother and larger due to previous erosion, reducing friction and gradient
What happens to gradient downstream?
In the River Severn the gradient decreases
- Weaker rock has already been eroded along the middle and lower courses, more resistant rock upland so gradient remains high,