Mindmap
Rivers
Inhalt der Mindmap
Rivers
The water cycle and drainage basin
- evaporation
- condensation
- precipitation
- infiltration
- when water filter though the ground and the tiny pores in the soil
- transpiration
- water evaporated from leaves
- throughflow
- rainfall/water flow through soil
- percolation
- water moves downwards through soil into saturated rocks
- surface storage
- precipitation retained on the ground surface
- groundwater flow
- deep movement of water through underlying rock
- soil moisture
- water is stored in soil
- infiltration
- precipitation
- condensation
- evaporation
river processes
- erosion
- the wearing away of the river bed and banks or the loads
- HYDRAULIC ACTION
- high velocity water pushes air into cracks on the banks
- ATTRITION
- loads bumping into each other and breaks
- ABRATION
- loads that are thrown against bed and banks causing them to be worn away
- SOLUTION
- acid and alkali dissolve the bed & banks
- transportation
- SUSPENSION
- particles supended in the river carried by its flow
- SALTATION
- pebbles are bounced along the river bed
- SOLUTION
- dissolved materials
- TRACTION
- big boulders bouncing along the bed
- the movement of the load down the river
- SUSPENSION
- deposition
- the laying down of a river's loads as its velocity decreases
- factors
- less water
- increasing amount of loads
- shallow
- recah its mouth
- drop its biggest load first
- erosion
river landscapes
- drainage basin
- source
- the start of a river
- tributary
- a small stream that joins a large river
- confluence
- where a tributary joins a large river
- an area of land drained by a river and its tributaries
- watershed
- the edge of a river basin
- mouth
- the end where a river joins the sea
- source
- long profile
- UPPER COURSE
- v-shape valley
- narrow
- shallow
- waterfall/gorges
- river flows over the hard resistant rock
- erodes the less resistant soft rock quickly
- abration and hydraulic action undercuts the hard rock leaving an overhung and a plunge pool
- overhang collapses
- repeated collapsing
- steep sided gorge
- river flows over the hard resistant rock
- interlocking spurs
- the river wind around the spurs because it's near its source and is not powerful enough to cut through the spurs so it has to flow around them
- MIDDLE COURSE
- gentle sloping valley
- wider/deeper
- meanders
- faster flow on the outside bend, slower flow on the inside bend
- faster flow : more energy and erosion, forming a river cliff
- slower flow : less energy and deposition forming slipp-off slopes
- over time erosion on the outside and deposition on the inside makes the neck becomes narrower
- swan's neck meander
- swan's neck part of the meander becomes filled with sediments, creates a straight path for the river
- ox-bow lake
- faster flow on the outside bend, slower flow on the inside bend
- river cliff
- slip off slope
- LOWER COURSE
- floodplain
- migrating meanders erode the sides of the valley
- wide
- migrating meanders leaves deposite of sand and clay
- flat
- migrating meanders erode the sides of the valley
- levees
- river breaks its banks
- deposit biggest loads firstalong the side of the river channel creating a levee
- river breaks its banks
- estuary
- where river meets the sea
- salt and fresh water mixes
- high tide
- incoming water stops the river flow
- deposites fine silts + sand that were in suspension
- making mud flats
- where river meets the sea
- floodplain
- UPPER COURSE
- drainage basin
flooding
- PHYSICAL FACTORS
- precipitation
- geology
- steep slopes
- HUMAN FACTORS
- urbanisation
- deforestation
- agriculture
- HYDROGRAPHS
- peak rainfall
- highest amount of rainfall
- rising limb
- how quickly discharge rises
- peak discharge
- highest recorded discharge
- lag time
- time difference between peak rainfall & discharge
- falling limb
- reduced discharge once run-off has passed
- base flow
- normal flow of a river
- bankfull discharge
- horizontal line : level of dischargeabove which flooding will occur
- peak rainfall
- BANBURY FLOODS
- impact of 1998 flood
- closure of railway station
- 12,500,000 pound worth of damage
- closure of shops and businesses, homes damaged
- FLOW CONTROL STRUCTURE
- low flow
- the weir control the flow
- medium flow
- upstream baffle controls the flow
- high flow
- downstream baffle controls the flow
- low flow
- EARTH EMBANKMENT
- the borrow area
- resevoir
- hardwick & huscote
- embankment
- storage area
- the borrow area
- impact of 1998 flood
- FLOOD MANAGEMENTS
- FLOOD RELIEF CHANNEL
- man made river channel
- FLOOD WARNINGS
- FLOODPLAIN ZONING
- land use restrictions on the floodplain
- FLOOD RELIEF CHANNEL
- PHYSICAL FACTORS