Paper 1: Rivers Flashcards
Source
The start of the river
Confluence
Point where two rivers join
Tributaries
Where the smaller river joins the main river
Watershed
Imaginary line which separate two drainage basins
Mouth
A river flows into the lake, sea or ocean
Upper course
Shallow
Slowest
V-shaped
Steepest
Middle course
Deeper
Faster
U-shaped
Flatter
Lower course
Deepest
Fastest
Open floodplain
Flattest
Erosion
Same four as coasts, only the processes act upon the river bank / bed
Transportation
Same four as coasts, but work from upper to lower course
Deposition
River will drop load when it loses energy
Interlocking spurs / v-shaped valley (UPPER COURSE)
The river erodes vertically and therefore is unstable
Gravity causes it to collapse = v-shaped valley
The process repeats, deepening the valley
As the river flows through the valley it is forced to swing from side to side (spurs)
Waterfalls / gorges (UPPER COURSE)
Waterfalls form when there is hard rock on top of soft rock
The soft rock is eroded through hydraulic action and abrasion
This leaves an overhang of hard rock which becomes undercut and collapses due to gravity; creating a plunge pool
Overtime the waterfall retreats due to headward erosion creating gorges (steep-sided river valleys)
Meanders (MIDDLE COURSE)
Lateral erosion widens the river
The current of the river is pushed towards the outside bend and therefore there is more erosion; hydraulic action and abrasion
The lateral erosion on the outside bend causes undercutting
Water on the inner bend is slower, causing material to be deposited creating a slip of slope
Ox-bow lakes (MIDDLE COURSE)
The neck of the meander has become narrower due to more erosion
The neck of the meander becomes cut through
Deposition seals off the end of the old meander
Vegetation grows in between the ox-bow lake and the river
Floodplains (LOWER COURSE)
Erosion removes any steep valley sides creating a wide flat area on either side of the river
During a flood, material carried by the river is deposited, building up the floodplain
Meanders migrating across the floodplain also makes it wider
Leeves (LOWER COURSE)
Leeves are natural embankments along the edges of a river channel
During a flood, eroded material is deposited over the whole floodplain
Estuaries (LOWER COURSE)
The water floods over the banks of the river carrying the silt and sand onto the valley floor
As the tide reaches its highest point, the water moves slowly and the sediment is deposited
Over time this builds up more, creating large mudflats
At low tides, the wide mudflats are exposed
River Tees
Location - North East
Source - Pennine Hills near Cross Fell (893m)
Mouth - Middlesbrough at the North Sea
Upper course landform - High Force waterfall and gorges
Middle / lower course landforms - meanders, levees and floodplains
Human factors causing flooding
Deforestation
Urbanisation
Climate change
Storage reservoirs
Physical / natural factors causing flooding
Relief of land
Prolonged or antecedent rainfall
Soil saturation
Climate change
Lag time (hydrograph)
How long it takes the river to fill up
Peak discharge (hydrograph)
Maximum amount of water flowing in a river
Rising limb (Hydrograph)
The rising flood water in the river