Rivers Flashcards
Formation of deltas
When a river reaches a sea energy is absorbed my slow movement of water of the sea.
This causes river to deposit its load.
Deposition builds up and partially blocks mouth of river.
River has to braid into several distributaries to reach sea
Formation of meanders
Alternating pools and riffles develop at equally spaced intervals.
Energy is lost from river when flowing over riffle due to friction
Spacing causes an uneven flow and to be concentrated on the one side
Turbence causes water to twist and coil- helicoidal flow
Cause more erosion and materiAl to be deposited on inside of the bend
Formation of levees
Natural raised embankments when a river overflows it’s banks.
Material is deposited during flood and river looses velocity due to friction.
Heaviest material drops first closest to river channel.
This builds up and forms a levee
Rejuvenation
When base level is lowered either by ground level rising or drop in sea level.
It increases vertical erosion and long profile is extended to a knock point
Formation of waterfalls
Soft rock meets hard rock and soft rock is eroded faster. This causes step in river bed.
Water flowing over step speeds up due to lack of friction adding to its erosive power. This causes undercutting of hard rock and will eventually collapse.
Deep plunge pool caused by abrasion and over time, further undercutting causes more collapsing so waterfall retreats
Suspension
Fine material carried by turbulence
Saltation
Larger particles bounce on river bed
Traction
Large particles rolled along river bed
Capacity
Total load that a river can transport
Location of Carlisle
North Cumbria
Date of Carlisle flood
8th January 2005
Causes of Carlisle flood
Heavy rainfall
Saturated ground
Steep sided drainage basin
Human causes of Carlisle flood
Urban area
Poor drainage and sewage systems
Social impacts of flood
3 deaths
3000 homeless
Stress related illnesses
Economic impacts of Carlisle
Repair cost £100 million and took a year
350 businesses shut down
70,000 homes lost power