Source: The point where a river begins
Drainage
Basin: The area of land that drained by a particular river and its tributaries.
Watershed:
The boundary or divider between two drainage basins, like the top of a house
rooftop
Course: The
route taken by a river as it flows down towards the sea or ocean
Tributary: A
smaller river that runs into a larger river
Confluence:
The point where two or more rivers meet
Mouth:
Where a river reaches the sea
Estuary: The
part of the river mouth that is tidal as it merges with the sea or ocean.
All rivers
have an upper, middle, and lower course.
In the Upper
Course the process at work is Erosion. The features you will see are Waterfalls, Rapids and a V shaped Valley
The upper
course begins in the hills or mountains. Here the river is smaller and usually
has a rapid,
tumbling
flow that cuts a narrow channel through rocky hills or mountains. It may roll
large boulders
along in
its swift current. The river can create waterfalls where it carves out layers
of soft rock and leaves a cliff of hard rock standing.
It forms
rapids along sloping rocky beds.
In the Middle
Course the process at work is both Erosion and Deposition
The features
you will see are Meanders, Oxbow Lakes
The middle
course of a river has more water than in the upper course. The slope is gentler
and flatter.
Erosion has
widened the channel. Deposition also occurs as some of the material eroded in
the
Upper
Course starts to settle. The river channel has also become deeper. Meanders are
typical
landforms
found in this stage of the river. Oxbow lakes can also occur when the river
cuts through the land in a straight line and cuts off the meander leaving it as
a lake.
In the
Lower Course the process at work is Deposition.
The volume
of water in a river is at its greatest in the lower course. This is due to the
contribution of water from tributaries. The river channel is deep and wide and
the land around the river is flat. Energy in the river is at its lowest and
deposition occurs.
A Delta is a feature often found at the mouth of a river. An example is the Nile Delta. Deltas are formed when a river deposits material faster than the sea can erode it. High banks called Levees can also be seen.
Upper Course of a river, featuring waterfalls and rapids caused by the process of erosion
Middle Course of a river, featuring meanders caused by the processes of erosion and deposition
Lower Course of a river featuring a Delta caused by the process of deposition.
River
Videos
A useful
video on what the ‘profile’ of a river looks like. The profile is what the
river would look like if we could see it from the side.
A nice song to remember the most important river features
and processes!
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