Zusammenfassung der Ressource
Rivers Topic
- Drainage Basin
- The catchment area from which a river
system obtains its water. An imaginary
line called the WATERSHED delimits one
drainage basin from another.
- Storm hydrographs
- FLASHY
- Short lag time
- steeper drainage basin
- lots of surface runoff
- underlying rock
- less percolation
- urban areas
- less trees
- less interception
- ploughing fields
downhill
- more tributaries
- SUBDUED
- Labelling
- lag time
- the time delay
between maximum
rainfall amount and
peak discharge.
- rising limb
- As the water enters the drainage basin
the discharge rises- there's a delay due
to overland flow and interception
- base flow
- the starting and finishing level
- receding limb
- shows the fall in the discharge back to the base level
- peak discharge
- indicates the highest flow in the channel
- type of hydrograph is determined by relief, rock and soil
type, vegetation, land use, weather, urbanisation,
drainage basin density, drainage basin shape and size
- Long profile
- River rejuvenation
- significant breaks in slopes (knick
points) along a river's long profile- may
be due to rejuvenation
- illustrates the changes in the altitude of the course of the river from
its source, along the entire length of its channel to the river mouth.
- UPPER COURSE
- LANDFORMS
- small waterfalls
- due to change in rock type
- rapids
- potholes
- large boulders
- uneven steep river beds
- TRANSPORTATION
- mostly large boulders
- some suspension
and little in solution
- PROCESSES
- hydraulic action, attrition, mostly vertical erosion
- DEPOSITION
- bedload is too heavy so limited deposition
- MIDDLE COURSE
- LANDFORMS
- rapids
- small meanders
- small floodplain
- PROCESSES
- lots of attrition
- little hydraulic action
- more lateral erosion-
start of meanders
- TRANSPORTATION
- less traction
- suspension increases
- DEPOSITION
- in slow waters
- floodplains
built in times
of flood
- LOWER COURSE
- LANDFORMS
- Large meanders
- levees
- floodplains
- PROCESSES
- erosion
reduced, just
small lateral
erosion
- slower waters
- TRANSPORTATION
- small bedload
- mostly suspension
- DEPOSITION
- mostly fine
particles,
- forms
levees, slip
off slopes
and
floodplains
- BRADSHAW MODEL
- PROCESSES
- EROSION
- Hydraulic action
- power of
moving water
removing
materials from
the channel
bed leading to
collapsing
- corrasion
- rubbing actions of material carried along the river bed
- corrosion
- minerals in rock dissolved by weak acids
- attrition
- particles striking against one
another into smaller pieces
- TRANSPORTATION
- Solution
- dissolved particles
- suspension
- fine materials (sand and
silt) carried in water flow
- saltation
- small stones bounce along the river bed
- traction
- stones and boulders roll
downstream in fast water
- Deposition
- Hjulstrom curve
- velocity and deposition
relationship shows
when particles are
eroded deposited or
transported in relation
to particle size