Process and impact of rejuvenation Flashcards
Rejuvenation meaning
to restore to a former state; to make fresh or new again
Dynamic equilibrium
where there is a balance between the rate of erosion and deposition
Dynamic rivers
Rarely ever, if ever, in state of dynamic equilibrium
changes in discharge and sediment load are constantly changing the profile of the river.
Base Level Changes
Eustatic change- changes to sea level
Isostatic change: Glacial rebound
Eustatic (global) change
Decrease in global temperatures causes more snow (precipitation), becomes ice so more water on stored on land.
Rise in temperatures melts ice and glaciers causing rise in sea level
Isostatic (local) change
RISE- glacial period, glaciers cause crust to sink lower into mantle
FALL- end of glacial period, ice melts, crust slowly rises, sea level falls
Causes of Rejuvenation
Tectonic Changes
Fall in Sea levels due to eustatic + isostatic changes
River capture
How does a river become rejuvenated?
- Renewed period of vertical erosion to achieve a newer and lower base level
- Fall in base level means river now has more energy to actively erode the irregularity.
- Over time river can achieve a state of equilibrium with a long, smooth profile.
How is a knick point formed?
Through a fall in base level
Retreats upstream over time like a waterfall
What happens when a river is rejuvenated?
~Adjustment to new base level starts at sea and works way upstream gradually.
River gains more cutting power (vertical), adjusts long profile
Effects of Rejuvenation
Renews river capacity to erode (increase in potential E)
Landforms as moves upstream:
- Knickpoint
- Waterfalls
- Rapids
- River Terraces
- Incised Meanders
What is a knick point?
a sudden break or irregularity in the gradient along the long profile of a river
What is a river terrace?
a remnant of former flood plain which has been left at a higher level after rejuvenation of river
Benefits of River Terraces
Provide useful shelter from floods in a lower course river valley and natural route ways for roads and railways.
How are river terraces formed?
- Lateral erosion
- Meander migration
- valley widened
- Deposition of sand and silt during floods