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Course Of River And Its Route
 Discussion about the course of river
 The general terminologies regarding river
 Erosion and its result on the shape of river
 The detail insight of the river pattern and its
final destination
 Summary of the entire presentation
 Question/Answer session
 A river is a natural watercourse, usually
freshwater, flowing towards an ocean, lake,
sea or another river
 Rivers can flow down mountains,
through valleys or along plains, and can
create canyons or gorges.
 Source of river
 Body of river
 Confluence
 Mouth of river
 Primary course
 Secondary course
 Tertiary course
 Origination from a mountain lake or a glacier
 V-shaped valley
 Water fall
 Hydraulic action
 Aberration
 Attrition
 Cascade
 Interlocking spurs
 Potholes
 The force of the water weakens and breaks up the
rocks
 ABRASION, The material carried in the river wears
away the river bed
 ATTRITION, As the pebbles carried by the river
crash into each other, they become smaller and
rounder
 SOLUTION, The water in the river dissolves the
minerals in the rocks
Rolling stones along the river bed.(
needs lots of energy)
Traction Suspension
Clay sized particles are carried
along by the river flow
Saltation
Sand sized particles
bounce along the riverbed
Solution
Some minerals are dissolved
by the riverwater
river flow
Formation Of A Waterfall
Soft rock
Hard rock
Steep sides
( gorge )
Vertical erosion
Forms plunge pool
Undercutting
erodes the
softer rock
forming an overhang
The overhang
Eventually
collapses
The process
starts again
Eroded rock
Waterfall
Retreats upstream
 Menders
 Ox bow lakes
 Flood plains
 Confluence
 MENDERS, Rivers snaking across and is
called mendering river or mender
 Ox-bow lake, Cut of region of a river is
called ox-bow lake
 FLOODED PLAINS, The area around a river
that is usually used for irrigation
 CONFLUENCE, The point where the
tributary joins the river
 Levee
 Mouth
 Deposition
 Delta
 Estuary
 Swamps, Marshes (mangrove)
 LEVEES, Is the natural or artificial banking
of a river to prevent out flow or river usually
due to erosion on bed
 DEPOSITION, The eroded material is
steadily washed into the ocean
 MOUTH, The area where the river meets the
sea
 DELTA, Is the area where the river splits into
a few portions and make a Δ shape
 ESTUARY, An estuary is a partly enclosed
coastal body of brackish water with one or
more rivers or streams flowing into it, and
with a free connection to the open sea.
 SWAMP, An area of low-lying, uncultivated
ground where water collects; a bog or marsh.
 MANGROVE, A tree or shrub that grows in chiefly
tropical coastal swamps that are flooded at high
tide. Mangroves typically have numerous tangled
roots above ground and form dense thickets.
Characteristics Upper Course Middle Course Lower Course
Slope
Width
Depth
Straightness
Load
Main work
Valley width
Type of load
usually steep
narrow
shallow
winding
little
large/small
angular
erosion
transportation
steeper
wider
deeper
meandering
some
medium/small
rounded
Transportation
narrow
gentle
quite wide
wide
deep
big meanders
lots
small+
rounded
transportation
deposition
wide
River   final

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River final

  • 1. Course Of River And Its Route
  • 2.  Discussion about the course of river  The general terminologies regarding river  Erosion and its result on the shape of river  The detail insight of the river pattern and its final destination  Summary of the entire presentation  Question/Answer session
  • 3.  A river is a natural watercourse, usually freshwater, flowing towards an ocean, lake, sea or another river  Rivers can flow down mountains, through valleys or along plains, and can create canyons or gorges.
  • 4.  Source of river  Body of river  Confluence  Mouth of river
  • 5.  Primary course  Secondary course  Tertiary course
  • 6.
  • 7.  Origination from a mountain lake or a glacier  V-shaped valley  Water fall  Hydraulic action  Aberration  Attrition  Cascade  Interlocking spurs  Potholes
  • 8.
  • 9.
  • 10.
  • 11.  The force of the water weakens and breaks up the rocks  ABRASION, The material carried in the river wears away the river bed  ATTRITION, As the pebbles carried by the river crash into each other, they become smaller and rounder  SOLUTION, The water in the river dissolves the minerals in the rocks
  • 12. Rolling stones along the river bed.( needs lots of energy) Traction Suspension Clay sized particles are carried along by the river flow Saltation Sand sized particles bounce along the riverbed Solution Some minerals are dissolved by the riverwater river flow
  • 13. Formation Of A Waterfall Soft rock Hard rock Steep sides ( gorge ) Vertical erosion Forms plunge pool Undercutting erodes the softer rock forming an overhang The overhang Eventually collapses The process starts again Eroded rock Waterfall Retreats upstream
  • 14.
  • 15.  Menders  Ox bow lakes  Flood plains  Confluence
  • 16.  MENDERS, Rivers snaking across and is called mendering river or mender  Ox-bow lake, Cut of region of a river is called ox-bow lake  FLOODED PLAINS, The area around a river that is usually used for irrigation  CONFLUENCE, The point where the tributary joins the river
  • 17.
  • 18.
  • 19.  Levee  Mouth  Deposition  Delta  Estuary  Swamps, Marshes (mangrove)
  • 20.  LEVEES, Is the natural or artificial banking of a river to prevent out flow or river usually due to erosion on bed  DEPOSITION, The eroded material is steadily washed into the ocean  MOUTH, The area where the river meets the sea
  • 21.  DELTA, Is the area where the river splits into a few portions and make a Δ shape  ESTUARY, An estuary is a partly enclosed coastal body of brackish water with one or more rivers or streams flowing into it, and with a free connection to the open sea.
  • 22.  SWAMP, An area of low-lying, uncultivated ground where water collects; a bog or marsh.  MANGROVE, A tree or shrub that grows in chiefly tropical coastal swamps that are flooded at high tide. Mangroves typically have numerous tangled roots above ground and form dense thickets.
  • 23. Characteristics Upper Course Middle Course Lower Course Slope Width Depth Straightness Load Main work Valley width Type of load usually steep narrow shallow winding little large/small angular erosion transportation steeper wider deeper meandering some medium/small rounded Transportation narrow gentle quite wide wide deep big meanders lots small+ rounded transportation deposition wide