rivers ποΈ Flashcards
(40 cards)
mouth
the point at where the river reaches the sea/lake
confluence
the point at which a tributary flows into another river
watershed
a ridge of high land that forms the boundary between 2 adjacent drainage basins
drainage basin
the area drained by a river and its tributes
source
the start of a river, it can be a hollow where water accumulates or a natural spring where water reaches the surface
tributary
a small stream that flows into a larger one
river
a large natural stream of flowing water that empties into another water body ( lake , sea other river )
the drainage basin system
precipitation
interception
evaporation
surface storage
infiltration
surface run off -( evaporation )
soil moisture storage -( through flow , channel flow )
percolation
ground water storage -( ground water flow )
transpiration
water stored on the plants / leaves turn into vapour and spreads into the atmosphere
why does the amount of interception vary from place to place
some areas have more vegetation than others
why does the amount of interception vary at different times of the year
trees shed their leaves in the winter if it rains / snows the water is able to get into the ground
river processes
erode, transport , deposition
erode
hydraulic action
attrition
corrosion
abrasion
transport
saltation
solution
traction
suspension
river long profile
shows a change in the height of the course of a river from its source to its mouth. al long profile is usually concave and the slope becomes more gentle towards the mouth of the river
upper profile
profile is steep
reduces hight very quickly
a lot of potential energy because of the steep drop
dominated by vertical erosion
narrow and steep sided
has little water volume
middle profile
the gradient of the profile has reduced
lateral erosion is more as more of the profile has reduced
lateral erosion is more important
the channel is wider and the valley sides are less steep
lower profile
less erosion , more deposition
potential energy has been replaces by energy from a high water volume
the river carries a large amount of load
waterfall
the softer rock retreats backwards upstream
the overlying then becomes unsupported and falls / brakes away
the fallen material gets swirled around in the plunge pool
meanders
a bend in a river
as the river gets more load it becomes more difficult to move along a straight channel
where the water hits the bank it erodes material in the areas where the water is travelling slower, the water has less energy and so deposits the eroded material
how are meanders formed
As the water flows around the bend it is pushed further out causing the water flowing on the outside of the bend to be faster.
This means that erosion takes place and the bank is undercut by the process of hydraulic action and abrasion. This forms a river cliff.
On the inside the flow is slower and therefore deposition occurs to form a slip off slope or point bar.
Potholes
If the river bends is uneven, pebbles become trapped in holes
Swirling currents cause the pebbles to rotate and erode circular holes in the river bed
This is done through the process of corrosion whereby sediment is trapped in the pot hole
Score away the base and the sides of it making it deeper and wider
Oxbow Lake
Before
Lateral erosion
Land being eroded on both sides
Deposition
Line of fast flow
After
Neck of land removed by erosion of the banks from two side sides often at the time of flood
Position use of the ends of the cut off lake
Stagnant water
Meander Island
Oxbow Lake
Rivercliff
Flood plain
A floodplain is an area of flat land either side of the river, which is often marsh. When a river floods it carries the load from the river onto the land either side. The big material is deposited first next to the river as it heavier. This builds up the banks making them taller these are called levees. The fine muddy material called alluvium is carried further. As the water seeps into the ground or flows back into the river, the sediment is left behind leaving the land much more fertile during normal flow the river deposits material from its load on the river bed causing the river to be lower than the surrounding floodplain.