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Connecticut Water Trails Association |
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Connecticut Water Trails Program Rivers
What Is A River ?
Rivers
A river is a natural stream of water which flows in
a channel towards a mouth or lake or another river. Rivers have two
banks (left and right bank). They have a bed over which the water flows.
Rivers always have a source, from where they start. Rivers always flow
downhill.
River Banks
Rivers have two banks - the right bank and the left
bank. If you stand in a river and face the way the water is flowing, the
right bank will be on your right hand side and the left bank will be on
you left hand side.
River Bed
The river bed is the bottom of the river. It can be made of stones, pebbles, boulders, rock and mud. The water flows over the river bed. You can see the river bed in streams, and in the upper course of a river, because the water is shallower. In the middle and lower courses of a river, you cannot see the river bed because the water is much deeper.
River Channel
The river channel is the course for the river water.
It can either be a straight channel like a canal, or a meandering
channel. The channel gives the river its shape. Courses
Of Rivers
Rivers have three courses. The course is the journey
the river makes to reach the sea. Rivers never have a straight course
from source to mouth. Their course is always bendy.
The upper course is found in the mountains and hills
where the river rises from its source. Often waterfalls and rapids are
also found in this course. The river is usually fast flowing in the
upper course. There are lots of stones and boulders for the water to
flow over. The river starts as a stream in the upper course and flows
through V-Shaped valleys.
The middle course is where the river starts to
become wider and deeper. The land which the river flows over is becoming
flatter. The river starts to meander or bend in the middle course.
The lower course is where the river becomes its
widest and deepest. This course is found closest to the sea where the
river has its mouth. The flat area of land by the river banks is known
as a floodplain. Farmers grow crops there. Sometimes a river can also
have an estuary or a delta as its mouth.
Stages
Of Rivers
There are also three stages to a river's life.
The River Source
The source is the start, or beginning, of a
river. The source of a river is usually found in the hills or mountains.
A river can have more than one source. The source is where a river
begins its journey.
Types Of Source
There are many different ways in which rivers
can begin:
Springs - Some rivers begin
where water flows out of rocks. Rainwater sinks through the soil and
trickles through the cracks and spaces in rocks such as chalk and
limestone. These are called permeable rocks. The water continues to do
this until it reaches a rock like clay. Clay is an impermeable rock.
The water gradually builds up between the
boundary of impermeable and permeable rocks. Eventually, it trickles out
of the rocks.
Rills and streams. - A lot of rain
falls on mountains. Rainwater flows down slopes and quickly makes
channels. At first the channels are small. They are called rills. These
join together to make bigger rills. Finally a stream is formed. The
streams join up to make a river.
Lakes
- The source of some rivers is a lake.
Melting snow and ice - Water
from a melting glacier may be the source of a river. The snow and ice
melt when the weather gets warmer. This forms a lake in front of the
glacier. The water rushes into channels in the V-Shaped valley and
eventually forms a river.
Bogs - In some places, rain
water can't sink into the ground as the ground is too wet already. The
water forms a bog. The soil and plants nearby soak up the water. The
water flows out of the bog to form lakes and streams.
The
River Mouth
At its mouth, the river flows into another body of water. The mouth may be where the river meets the sea, a lake or a larger waterway. Most rivers flow out into the sea, and this is where they end their journey.
Not all river mouths are the same. There may be an estuary or delta at the mouth. Not all rivers enter the sea. Some rivers simply dry up.
The 'mouth' is where the river
stops flowing.
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