rivers Flashcards
(37 cards)
drainage basin
an area drained by a river and its tributaries.
Lateral erosion
sideways erosion
Evaporation
water heated turning from a liquid to a gas (water vapour)
Erosion
the wearing away of the land
abrasion
material carried by the river smashes against the banks wearing them away
attrition
rocks smashing into each other gradually become smaller and rounder
hydraulic action
the force of the water and/or forces air into cracks making them wider
solution
where water has a chemical reaction with the rock and dissolves it
suspension
lighter material is carried in the river.
solution
dissolved material transported
saltation
heavier material is bounced along the bed of the river.
traction
the heaviest material is rolled along the bed of the river.
deposition
when material is dropped by the river
take place where the velocity of the river slows down for example on the inside of a meander, at the mouth where the river meets the sea, or on the floodplain when it overflows.
name the 3 processes
erosion, transportation and deposition
name the 5 landforms
v-shaped valleys, waterfalls, meanders, oxbow lakes, floodplain
how does the river change from upper to lower course
River becomes wider
Discharge increases
Velocity increases
Gradient decreases
why does a river change from upper to lower course
River becomes wider - as a river reaches its lower course lateral erosion becomes more common, as gradient decreases, widening the river.
Discharge increases - as more tributaries join the river amount of water increases.
Velocity increases - as bedload has become smaller and banks and bed smoother friction decreases therefore increasing velocity.
Gradient decreases - due to meander migration widening the valley floor
Interlocking spurs
The river at its source is small and has limited energy. It flows naturally from side to side around ridges of more resistant rock creating spurs.
v-shaped valley
vertical erosion takes place deepening the channel whilst weathering attacks the slopes, weakening the rock until mass movement moves the material downslope.
waterfall process
Hard, more resistant rock overlays softer less resistant rock. Soft rock is eroded more rapidly through hydraulic action/corrasion undercutting the hard rock creating an overhang. The force of the water creates a plunge pool. The hard rock collapses under its own weight and the process repeats, retreating upstream to create a gorge.
process of meanders/oxbow lakes
Water flows fastest on the outside of a meander eroding the banks, creating a river cliff. On the inside of the bend where the river is flowing slower deposition takes place creating a slip-off slope. As erosion continues at the neck of the meander it becomes narrower. Normally in flood conditions the force of the water breaks through creating a new channel. The old part of the river is cut off as deposition now takes place along the banks of the river, creating an oxbow lake.
flood plain
the floodplain is a wide flat area of land either side of the river. In its lower course meander migration takes place. This occurs due to lateral erosion eroding the outside of the bend and deposition on the inside moving the meander across the valley floor, widening and flattening it.
what were the physical causes of the Boscastle flood
Intense rainfall, 185mm in 5 hours, did not allow time for water to infiltrate therefore overland flow increased.
Large amount of rainfall earlier in the week and an input of 3 million tonnes of water meant ground was saturated and could hold no more water.
Confluence of 3 rivers, Valency, Jordan and Paradise drained a small drainage basin of just 40Km2.
Geology - impermeable sandstone did not allow water to infiltrate and therefore overland flow increased.
Steep valley sides reduced infiltration and thin soils couldn’t hold much water
what were the human causes of the boscastle flood
Narrow bridges became blocked with trees diverting water into the streets.
Deforestation results in fewer trees to intercept and store water . Therefore more water gets to the river channel.
Urbanisation results in water flowing rapidly into drains over impermeable surfaces. The water gets to the river channel too quickly.