Own Knowledge - Rivers Flashcards
(36 cards)
types of weathering
physical - freeze thaw
chemical - acid rain
biological - roots of plants
types of mass movement
sliding
rock fall
slumping
types of erosion
hydraulic action - sheer force of the water
abrasion - material carried by the river being rubbing against banks and bed of the channel, wearing it away
solution - minerals dissolve into water - slightly acidic - dissolve rocks
attrition - sediment particles collide with each other - rounder and smaller
types of transportation
traction - rolling along river bed
saltation - bounce over eachother on the river bed
suspension - the water flow carries silt and clay-sized particles
solution - river water dissolves some minerals
how do interlocking spurs form
- upper course
- erode downwards
- flow around the hardest parts of the rocks
how do waterfalls form
- band of hard more resistant rock lies over a band of soft rock
- river erodes less resistant rock at a faster rate - undercutting it
- eroded by hydraulic action and abrasion
- hard rock overhangs
- hard rock falls under force of gravity
- falling rocks cause erosion of the river bed and the formation of PLUNGE POOL
- gorge forms as waterfall retreats = soft rocks eroded and hard collapses - gorges form in hard rock where vertical erosion is dominant
how do meanders form
- found in flood plain
- highest velocity on outside of the bend - lateral erosion
- forms a RIVER CLIFF
- inside of bend - velocity less - deposition
- forming a POINT BAR
how do oxbow lakes form
- rivers erode outside of bend fastest
- narrows the neck
- eventually erodes through neck
- new river by passes the meander
- dries up leaving an oxbow lake
how is a flood plain formed
- formed by both erosion and deposition
- lateral erosion on outside of bends of meanders means they MIGRATE across valley floor + erode Vally sides = valley floor becoming wide and flat
- during floods - flood water spreads across valley floor + deposit fine sediments called ALLUVIUM as it loses energy - flat land
how do levees form
- natural embankments of sediment on either side of a river
- during a flood water come out of channel and lose velocity
- deposits the larger + heavier material first on its bank
- repeated flooding causes these banks to get higher - forming levees
how do deltas form
- when rivers meet another body of watet eg. ocean - loses velocity + deposits sediment
- if river deposits faster than it erodes = sediment builds up in a fan-shaped DELTA
how does width change from source to mouth
- increases
how does depth change from source to mouth
increases
how does velocity change from source to mouth
increases
how does discharge change from source to mouth
increases
how does gradient change from source to mouth
decreases
how does channel roughness change from source to mouth
becomes smoother = less friction
how does sediment size change from source to mouth
becomes smaller + rounder
define lag time
the difference between peak rainfall and peak discharge
flashy hydrograph
- steeper rising limb
- short lag time
- higher peak discharge
subdued hydrograph
- gentler rising limb
- longer lag time
- lower peak discharge
how does drainage size and shape affect hydrograph
- small, elongated = higher discharge
- circular = lower discharge
bridging points on river severn
Shrewsbury
antecedent conditions - river severn 2007
140mm - highest in 100 years