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PUBLIC LIBRARY FORT WAYNE AND ALLEN COUNTY, IND
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RIVERS Irving
and Ruth Adler
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The John Day Company
— New
York
:
Books by Irving and Ruth Adler
NUMBERS OLD AND NEW
FROM TOPS TO ATOMS
THINGS THAT SPIN:
SHADOWS THE STORY OF A NAIL
WHY? RIVERS
Books by Irving Adler
FROM SPACE HOT AND COLD WEATHER IN YOUR LIFE
SEEING THE EARTH
DUST
THE TOOLS OF SCIENCE
THE SUN AND
ITS
FAMILY
MAN-MADE MOONS MONKEY-BUSINESS
HOAXES IN THE NAME OF SCIENCE
HOW
LIFE BEGAN
MAGIC HOUSE OF NUMBERS
THE STARS: STEPPING STONES INTO SPACE TOOLS IN YOUR LIFE FIRE IN
YOUR LIFE
TIME IN YOUR LIFE
THE SECRET OF LIGHT
© 1961 by Irving and Ruth Adler must not be reproany form without permission. Published by The John Day Company, 62 W^est 45th Street, New York 36, N.Y., and on the same day in Canada by Longmans Green & Company, Toronto. All rights reser\ed. This book, or parts thereof,
duced
in
Library of Congress Catalogue Card Number: 61-12714
Manufactured
in the
United States of America
U. SL 1254553 Contents Rivers
4
How Rivers Are Bom
6
Currents
8 9
Weathering
Wearing Away Mountains
10
VaUeys
12
The Grand Canyon
of the Colorado
14 16
Waterfalls
Water Gaps
18
Natural Bridges
20
Potholes
21
Treasure Hunting
22
Watersheds and Divides
24
Rivers That Are Pirates
26
The Lower River
28
Meandering
30
A River Changes Its Bed A River Changes Its Face
32
Taming Making
a
33
Wild River
34
36
Electricity
Rivers and Travel
38
Where People Live
.
40
*
Water Water
for Plants
.>
42
42
for People
Keeping Water Clean
43
Deltas
44
The Journey
Word
List
of a
Drop
of
Water
46 48
Rivers
^
This
is
a book about rivers.
Rivers are important for people. Rivers are important for plants
and animals,
Rivers help living things in
The water
that people
many
too.
ways.
and animals
drink often comes from rivers.
Some
of the fish that people eat are
taken from
rivers.
Many plants are used by people as food Growing
plants
need water. In some
places rivers help bring water to the land
where the plants grow. Rivers are natural roads. People use boats, barges
and
from one place
rafts
to carry things
to another along a river.
Rivers help people in other ways, too.
.^^
Rivers turn water wheels, making the machines in mills and factories work. Rivers
turn the machines that
make
electricity.
Rivers can help people enjoy their free time.
Some people
Many
boating.
most everyone
like to
people
go fishing or
like to
swim. Al-
likes to look at the pretty
scenery along a
When
rivers
flood their banks, they can carry
away
Rivers can also do harm.
people's
X
river.
homes and belongings.
we shall find out how rivers We shall see how rivers go down
In this book are born. to the sea
and what they do
they go there.
work
to
We
change
to the land as
shall see
how
people
rivers so that rivers will
always be helpful friends.
Pi^^ \
Ground
^
^ — ^
water \
i
\ ..
:
,
,
,
•:.::•>/
\
.
Spring Spring water flows downhill into the stream
^^V/ uiut I
.
Ground^:^^
'•^-:^^V:^^:'•:•^:-:^•:v^ntothe^sti^ai^t/^•^^
vr^.
Hoti; Rivers
Rivers are born high
up
Are Born
in the mountains,
from rain
and melted snow.
is
Much
of the rain that falls sinks into the earth. This
called
ground water. Some of
this
water flows out of
the ground again through openings in the rocks.
ground water comes out again
like this it
is
When
called a
The spring water then flows downhill and joins other springs to make streams. The streams also get ground water that goes into them right from the ground. Some rain flows downhill right away. The rain water spring.
flows along gullies
there is
is
and ditches
a lot of rain, the streams
no rain
for a long time,
When When there
into the streams.
become
full.
some streams dry
up.
Ground
water keeps other streams flowing even in dry weather. 6
In the wintertime,
snow piles up on the mountain tops. snow melts. Some of the melted
In the springtime the
snow sinks into the ground and becomes ground water. Some of the melted snow flows downhill into the streams right away. So, in the springtime when the snow melts, the streams are fuller than they are at other times.
They
are fuller in the spring, because a lot of rain
falls
then, too. In the mountains there are places that are
big bowls. Rain and melted snow
shaped
like
places,
making mountain
lakes.
When
fill
these
the lakes are
full,
the water begins to flow out of them. This water makes little
streams which go
down
the mountainside and join
other streams.
The mountain streams are the beginnings of rivers. The beginning of a river is called the upper river.
USOA Photograph
A mountain
lake
Currents If
there
is
snow on the ground, you may be able
coasting on a sled. hill is steep,
You
start at the
you coast down
not steep, you coast
down
it
it
more
you downhill. Gravity makes you ground
is
top of a
very quickly.
steep,
steep,
hill. If
If
the
go
the
hill is
slowly. Gravity pulls
travel faster
where the
steeper.
Gravity makes water flow downhill, too. is
to
If
the
hill
down it quickly. If the hill is not down it more slowly. But the sides of
water flows
water flows
a mountain are steep. So gravity makes the water in a
mountain stream flow
fast.
We
say that a mountain
stream has a fast current (CUR-rent).
U.S. Forest Service
A
fast flowing mountain stream
U.S. Geological Survey
Pile of smaller
rocks
made by weathering
Weathering Mountains are made up of
But they can be broken water and weather,
air.
it is
When
rock.
Rocks are very hard.
into smaller rocks
rocks are changed this
and
soil
way by
by the
called weathering.
Here are some ways weathering happens. If
you pour boiling water
into a cold glass, the glass
may break. If you fill a hot glass with ice water, the glass may break, too. The change from hot to cold, or from cold to hot, makes the glass crack.
Some
rocks
become
very hot during the daytime and very cold at night. The
change from hot
to cold, or
from cold
to hot,
makes the
rocks crack, too.
Rain and melted snow
becomes very
cold, the
When water freezes,
it
fill
the cracks in the rocks.
If it
water in these cracks freezes.
takes
up more
space. This
makes
the cracks bigger, and the rocks split into smaller rocks.
Wearing, Away Mountains
Flowing water slowly wears mountains away. ens the rocks and the
and
carries
them great
that weathering has
soil
distances. This
is
It loos-
made,
called erosion
(ee-ROW-zhun). As a stream flows down a
and sometimes ground
and
is
A
fast
It
sometimes
the ground
such a heavy load.
flows fast
where the
stream picks up rocks, stones
is
It
not so steep, the stream slows is
not strong enough to carry
drops some of the rocks and stones
has been carrying. But the stream
enough
it
flows fastest
flows along.
down. Then the stream
it
hill,
slows down.
steepest.
soil as it
Where
it
is still
sand and
moving
fast
soil. If
the ground
becomes steeper again, the stream can carry a
larger load
of rocks
to carry small bits of
and stones once more.
USDA Photograph
Land worn away by
rain water
U.S. Bureau of Reclamation
Footprints of a dried up stream
The beds
of
mountain streams and
rivers are
covered
with rocks. These rocks were carried along, and then
dropped, by the water. Some mountain streams dry up in the
summertime.
We
can
still
find their beds even
though the streams are no longer
have
left their footprints
there.
behind. There
is
and stones which the streams dropped
a
The streams trail
of rocks
as they flowed
along.
Streams drop
When more
many
stones at the foot of steep
hills.
they leave the mountains and travel slowly along
level ground, they also
they carry. 11
drop some of the
soil
that
U.S. Forest Service
The V-shaped
valley of the Colorado River
Valleys
The
sides of a
many httle hill in it
mountain are not smooth. They have
Mountain water
ditches.
these
little
ditches.
starts its trip
As the water flows downhill,
makes the ditches deeper and wears away
The
ditches begin to look like the letter V.
their sides.
Mountain
streams join with other mountain streams to river.
The V-shaped
which the
When
river flows,
the river
is
from the bottom of
is
it
picks
V-shaped
valley deeper. Rain water wears valley. This
makes the
a
other
V. This V,
called a valley (VAL-lee).
young,
its
make
come together with
ditches
V-shaped ditches to make an even bigger in
down-
soil
valley. This
away
valley wider. 12
up
and stones
makes the
the sides of the
When
the valley
is
wider,
its
the river
sides are not as steep. After a long time,
is
old, the valley
is
broad and
flat.
Then
when
it is
no
longer shaped like a V.
Some
river valleys
have been drowned by the
sea.
When this happens, sea water flows part way up the river valley.
So the river valley
is
hidden under sea water. This
Hudson River below the city of Albany, New York. That is why the Hudson River is salty all the way up to Albany, 150 miles away from the sea. The valley of the St. Lawrence River is drowned as far as Montreal. Delaware Bay and Chesapeake Bay are also drowned river valleys.
has happened to the
Chesapeake Bay before drowning
as
it
looks
now
U.S. Forest Service
The Grand Canyon
A and
valley its
called a
canyon (CAN-yun)
sides are very steep.
in places
not
is
of the Colorado
where the weather
is
deep
very dry. Then there
much rain water to wear away the
So, while the river
if it is
Canyons are usually found
makes the
is
sides of the valley.
valley deeper, the sides of
the valley stay steep.
The Colorado River is in the western part of the United States. It has made the largest and most beautiful canyon
in the world.
A
long time ago 14
this
land was
flat.
Many the
layers of different kinds of rock surfaces.
flat
make
its
Then
were underneath
the Colorado River began to
valley.
As the valley got deeper, the
different layers of rock
have different
began
to show. Different kinds of rock
colors.
So the sides of the valley have layers of
different colors.
The valley also kept Grand Canyon is ten
some places the the top and one mile deep.
Some
of the rock layers of the
softer than others.
They
harder layers. That
is
are
miles wide across
Grand Canyon
worn away
why the sides
many
getting wider. In
of the
are
faster than the
Grand Canyon
look like a big staircase.
The Colorado River at the
is
a
young
river. It is still at
bottom of the Canyon, making
The rock
its
work,
valley deeper.
layers look like a big staircase
Waterfalls
A
stream sometimes passes from a harder rock to a
wears away the softer rock more quickly.
softer rock. It
This makes the bed of the stream steeper and steeper.
Then
the water doesn't flow over the bed any more.
shoots over
The
its
bed
softer rock
in rapids.
underneath the river keeps wearing
away. Finally the river bottom
Then falls
of the Niagara River
water
is
so steep that
the water falls to the lower level. This
The shape still
It
a
cliff.
how
the
were made.
of the Niagara Falls
wears away the
it is
is
soft rock
is still
under the
the hard rock on top crumbles, too.
The Then
changing. river.
From time
to time
large pieces of rock at the top tumble into the water
below. So the
falls
Rapids
are slowly
moving upstream.
Waterfalls
The Niagara Falls are beautiful because they are so wide. The Falls are shared by the United States and Canada.
On the Canadian side they look like a horseshoe
a half mile long from end to end.
The
Falls are
about
160 feet high.
N.Y. State
The Niagara
Falls
Power Authority
Water Gaps
The rock
layers of the
Grand Canyon
of the Colorado
River are like layers of a layer cake. They are horizontal (
hah-rih-ZON-tull )
straight shelf.
,
or level. Sometimes rock layers are
up and down,
rivers cut their valleys
Some
may be
books standing on a library
vertical
soft, just like
easily than
soft layers.
where the
it
VUR-ti-kul )
Some
.
may be hard and some
the horizontal layers of the
river cuts
river valley gets
(
through vertical layers of rock.
of the vertical layers
Canyon. So the
more
like
These layers are
through the
Grand
soft vertical layers
cuts through the hard layers.
The
wider where the river has cut through
The
river valley stays
river has cut
steep part of the valley
Stream
How
through hard is
narrow and steep layers.
The narrow,
called a water gap.
Stream
a water gap
18
is
formed
Water
r
The Delaware River has made the states of Pennsylvania and
ware Water Gap
is
a water gap between
New
three miles long.
Jersey. Its
The Dela-
steep sides are
1,400 feet high.
Water gaps
are also called narrows.
U.S. Geological Survey
The Delaware Water Gap
Natural Bridges In Virginia there flows 200 feet
A just
is
a natural bridge of rock.
A
stream
below it. The stream has made the bridge.
long time ago there was a waterfall in the stream
below where the bridge
is
now. There was a large
crack in the rocky bed of the stream, above the waterfall.
Stream water flowed into the crack and came out again at the
bottom of the
falls.
The water made the crack larger and larger. Then became so large that all the water of the stream flowed through it. So a new waterfall was made
the crack
upstream.
The water
of this waterfall flowed
under the rock
where the old
falls
had been. The opening under the
rock of the old
falls
kept getting bigger and bigger. At
the same time, the Finally, all that
new waterfall
was
left of
kept moving upstream.
the old waterfall was a rocky
bridge over the stream that built
How
a natural bridge
is
it.
formed
U.S. Geological Survey
U.S. Forest Service
A
Natural Bridge of Virginia
pothole
Potholes
Sometimes a rock
will look as
though a big ice-cream
scoop has been at work making holes in holes are called potholes.
have been
at the
Water which
They
tell
These scoop-
us that the rock
bottom of a waterfall or under
falls
rapids hits the rocks
may
rapids.
from a great height or shoots down
below with a
lot of force.
bottom, the water turns and spins very carried
it.
fast.
The
At the stones
by the water spin around with the water. They
grind out the potholes in the rocks at the base of the or under the rapids. 21
falls
Treasure Hunting
Streams and rivers have
made
it
easier for miners to
find gold.
Gold
is
sometimes found in rock. But
it is
hard to get
The job of the gold miner is made easier when nature does some of the work for him. As rocks with gold in them are worn down by weathering, bits of gold break at there.
off
with
bits of rock.
Flowing water
carries these bits of
gold and rock downstream. As they
rub against each other. In
and polished. The
way
along, they
they are smoothed
rock that have been smoothed
bits of
are called pebbles.
this
move
Many
pebbles together are called
gravel.
Gold
is
heavier than gravel. So the lighter pieces of
gravel are carried farther downstream than the gold.
The heavier gold bottom of the
is
river
dropped upstream.
bed with
Gravel beds where gold (
PLASS-irs )
.
is
It settles at
the
larger pieces of gravel.
found are called placers
Taking gold from placers
is
called placer
mining.
The gold miners
of 100 years ago separated bits of
gold from the gravel of placers by panning. The miner
put
bits of
gold and gravel from the river bed in a shal-
low, round iron pan.
He
He then let water flow into the pan.
shook the pan at the same time. The shaking sepa22
rated the heavier bits of gold from the Hghter gravel.
Then
the gravel could be poured
oflF
with the water,
leaving small lumps of gold in the pan.
Most So not
of the gold in placers has already
much
placer mining
is
been found.
done any more.
U.S. Geological Survey
Placer mining
Watersheds and Divides
Two end
drops of rain that come from the same cloud can
their trip to the sea thousands of miles apart. This
happens
in
South America. The Juruena River and the
Paraguay River both apart.
start in Brazil
only three mile
There they have only a small mountain
between them. Water flows down one
(rij)
We say that this side of th.
ridge into the Juruena River. ridge sheds
its
water into the Juruena River. So
of the Juruena watershed.
rid^
side of tf
it is
part
The other side of the mountain
sheds water into the Paraguay River. So
it is
part of the
Paraguay watershed. The ridge between the two watersheds If falls
is
called a divide.
a rain cloud
from
it
is
over the divide some of the rain that
some also The Juruena River flows Amazon River. The Amazon River
flows into the Juruena River. But
flows into the Paraguay River.
north into the great
.
.
.
some goes
into
the ocean here.
.
Juaruena Rjver Of the
rai
that falls h^re
ParaeuayFiver
na River
and some goes he ocean here
into
empties into the Atlantic Ocean. The Paraguay River flows south into the Parana River.
The Parana River
empties into the Atlantic Ocean, too.
It
Atlantic
Ocean 3,000
empties into the
Amazon apart may
miles from where the
does. So raindrops that fall only three miles
reach the sea 3,000 miles apart.
Some watersheds
are very large.
The watershed
of
the Mississippi River covers almost half of the United States. All the
sippi River
is
that sheds
its
land that sheds
The
water into the Missis-
water into the rivers that flow into the
Mississippi River
called
its
in the Mississippi watershed. All the land
is
in the Mississippi watershed, too.
rivers that flow into the Mississippi River are its
tributaries
(
TRIB-you-ter-rees )
The Mississippi watershed
Rivers That Are Pirates
Men who
the seas and rob other saiHng ships are
sail
called pirates. Rivers are sometimes pirates, too.
become
pirates
when
They
they capture the waters of other
rivers.
The
pictures
on
this
tured some of
page show how the Shenandoah
became a pirate when it capthe water of the Beaverdam Creek in the
River became a pirate.
It
Blue Ridge Mountains of Virginia.
The Potomac River and
the
Beaverdam Creek both
used to flow through water gaps in the Blue Ridge Mountains. The
first
picture shows
what they looked
The Potomac River was stronger than the Beaverdam Creek. It cut its valley faster. So the valley of the Potomac became deeper than the valley of the
like then.
Beaverdam.
The Shenandoah River flows into the Potomac River. The head, or beginning, of the Shenandoah River was on one side of a divide. The head of the Beaverdam
Water
Creek was on the other side of the divide.
The Shenandoah flowed
into the deeper valley of the
Potomac. So the Shenandoah flowed faster than the
Beaverdam. Because
it
flowed
Shenandoah
faster, the
River was stronger than the Beaverdam Creek.
Both
rivers kept
wearing away the divide between
them. The stronger Shenandoah wore away quickly. Finally the divide
The path
its
was worn away
a river follows
is
called
its
flowing into the Beaverdam.
Shenandoah River
more
altogether.
The Beaverdam
channel.
Shenandoah channel was steeper than the channel. So the head of the
side
Beaverdam Creek stopped It
began
to flow into the
way
the Shenandoah
instead. In this
became a pirate which beheaded the Beaverdam Creek. The head of the Beaverdam Creek used to flow through a water gap. But water does not flow through the old
Beaverdam water gap any more. The water gap has become a wind gap. The second picture shows what the rivers look like
Wind gap
now.
The Lower River After a river leaves the mountains,
becomes the
river.
slopes a flat.
it
The lower river may flow over land that Or it may flow over land that is almost So the lower river flows more slowly than the upper
lower
river.
little bit.
Because the river has slowed down so much,
cannot carry the load of sand and
soil it
had when
it
it
left
the mountains.
When land that
a river flows is
very
drops most of layer of sand
its
and
flat,
down from steep mountains onto it slows down very quickly. So it
load of soil
soil
once.
The
been dropped looks
like
and sand
that has
all at
U.S. Geological Survey
A fan
Some fans are very large. The Merced River down from the high Sierra Nevada Mountains in
a big fan. flows
Cahfomia.
As the
fan
Its
more and more and
soil
is
river flows
80 miles through
of the sand
lower valley,
its
and
dropped along the
are
across. it
loses
The sand
soil it carries.
river bed.
In the springtime, heavy rains and melted snow
fill
the
They make the river spill out over its banks into the is called a flood (flud) The floodwater picks up soil and sand from the river bottom and spreads some of it over the valley land. The valley land is called the river.
valley. This
.
river's flood plain.
After a long time the flood plain
covered with a deep layer of sand and soil
soil.
have many chemicals (KEM-i-kals)
is
The sand and
in
them. These
chemicals were in the rocks in the mountains. They were
washed out Growing
of the rocks
when
the rocks weathered.
plants use these chemicals as food. So the land
of a flood plain
is
fertile (FUR-till), or rich in
At the same time, heavier
been dropped
in
bits of
plant food.
sand and
low ridges along the
soil
river banks.
ridges are levees (LEH-vees). These levees are
have
These
made by
nature. So they are called natural levee's. Natural levees
build up higher and higher each year. times ten or fifteen feet high. valley
from
floods.
29
They
They help
are some-
protect the
Meandering
The lower
river looks like a big snake
many bends and the time.
looks
all
looks
when
turns. It keeps
The lower
loses old
it
because
it
has
changing the way
it
way
it
river
changes the
bends and makes new ones.
Engineers (EN-jin-eers) wanted to find out
why
the
lower river bends and turns. They found that the bends
and turns are made by the
soil
and sand that the
river
They found this out by doing an experiment. They made a model of a river with a straight channel. They built the channel out of sand. They found that as carries.
soon as water flowed through the channel, the model river
began
tures
on
The
this
first
bend or meander (mee-AN-dur). The
to
page show how
this
happened.
picture shows the straight river channel.
Straight channel
The y^
river
wore away
the bank here
PBBI
.and built a sand bar here
30
pic-
The second first
began
picture shows the channel
to flow
wore away the carry
away
quickly as
it
at B, a little
at
began
bank
it.
The water But the
at A.
wore away. So
soil
below A. This made a sand bar at
to flow
B made
at B.
the river began to flow
at C.
the bank at C.
The
more
quickly,
third picture shows
way
ing
up sand bars along the whole
the water kept wearing
big snake, with
it
wore
what hap-
pened at C. But then another sand bar was made this
like a
as
more quickly between the sand bar
When
looked
bank
the river narrower. So the
the
bank
channel
and sand were dropped
B and
away
in the
river could not
the bits of soil and sand from the
The sand bar river
through
river
when water
at
away banks and
D. In
build-
river. Finally the river
many bends and
turns.
Then the river wore away the bank here
—
and built another sand bar here
31
A River'Changes Its Bed The Yellow River of China It
flows 15 feet above
very is
its
an old meandering
flood plain.
30 feet above the
river.
When the river is When the river
plain.
it may break through one of its natural levees. may leave its old bed below the break and make
so high,
Then a
full, it is
is
it
new
channel.
For 500 years before 1852, the Yellow River had been flowing into the Yellow Sea. After a flood in 1852, the
Yellow River changed of Pe-chi-li,
its
bed.
It
began
to enter the Gulf
250 miles north of the Yellow Sea.
The floods
of the Yellow River
In 1887 a million people were
have been very
drowned
terrible.
in a flood.
The
Yellow River has been named "China's Sorrow."
make the channel of the Yellow River deeper and straighter. They hope The Chinese government
that this will keep
it
is
trying to
from flooding and from leaving
bed.
?rtto
the sea here
its
A
A
river that
River Changes
Its
Face
meanders keeps changing
banks along one meander
may be
along the meander that came before
wears away the the second one.
first
meander
The
first
its
it.
faster than
The
So the river it
meander comes
closer to the second one. After
looks.
harder than the banks
many
a small strip of land between them.
wears away closer
years, there
Then
it is
is
and only
easier for
the water to flow across this strip of land than to flow
around of
it.
The meander is cut off, and the river The meander that has been cut
bends.
its
narrow,
like a long,
swampy
lake. It
is
loses
one
off looks
called a
bayou
(BYE-you). Cutoffs river
is
river.
happen more
easily during floods.
When
flooded, the water flows over the banks of the
Then
it
can easily wash away the narrow
strip of
land between two meanders.
Before a meander is
a
cut off
After a meander is cut off
Taming a Wild River Most
of the time
meandering
rivers are very quiet
and harmless. But they may become very dangerous.
They may
flood their broad valleys.
Then they may
kill
people and animals and carry away houses.
When
a lot of rain
falls
or
snow
melts, the water in a
keep the
river rises. Usually the natural levees
overflowing
banks. But sometimes the river channel
its
has to carry so
much water
levees anyhow.
Then
Farms, towns and
that the water flows over the
the river floods
floods.
The
rivers
One way to tame
its
have been
cities
valleys of large rivers. So the valleys
from
from
river
valley.
built in the fertile
must be made
safe
must be tamed.
a river
by building
is
levees along
its
banks. Hundreds of miles of levees have been built along
the banks of the Mississippi River and
Another way to tame a
When meanders shorter. This
are cut
makes the
river
is
its
the path of the river
off,
river flow faster.
can carry more water. So
tributaries.
by making
it
doesn't rise
cutoffs. is
Then the
made river
as high during
floods.
When to
a river wears
away
meander. Protecting the
tame a
river.
Mats made
its
river
banks, the river begins
banks
of concrete
is
a third
way
to
and heavy wire are
placed over part of the river bed. They go from the shore 34
a 1254551
a:
to the deepest part of the river channel.
A
fourth
way
across the river.
to
tame a
river
is
by building a dam
When there is a heavy flow of water into
the river, the water collects in a large lake behind the
dam. Then the is
stored
is
river does not rise.
A lake
in
which water
called a reservoir (REZ-ur-vwar).
A
levee near
New Orleans
Mississippi River
Protecting banks with concrete mats
Commission
Making
Electricity
made at electric power plants. The machines that make electricity are called generators (JEN-ur-ay-tors). Some power plants use the power of steam to turn the generators that make elecThe
electricity
people use
is
Other power plants use the power of flowing
tricity.
water to make
electricity.
In some places there
flowing water. In these places electricity
is lots
of
made by water
is cheaper than electricity made by steam power. One of the first power plants to use flowing water to make electricity is at Niagara Falls. A tunnel was dug
power
from the bed of the
river
above the
the river at the bottom of the
falls.
falls to
the bed of
Very strong water
wheels, called turbines (TUR-bins), were placed at the
bottom of the tunnel. Water
falling
through the tunnel
River
Water falls through the tunnel
.
The turbine turns the generator,
.
making
and makes the turbine turn very fast
How
electricity
Water flows into the river again
water power makes electricity
U.S. Bureau of Reclamation
Grand Coulee Dam
made the turbines
turn very
fast.
The
turbines were con-
nected to electric generators. So the electric generators turned, too,
A new
making
electricity.
power plant which uses the water of the Niagara River was finished in 1961. It is the largest electric
plant run by water
power
in the
Water flowing over a dam
is
United
States.
like a waterfall. It
used to turn turbines which are connected to generators. There are electric
Coulee
Dam
power
Hoover
Dam
State
and
dams
are used to prevent floods, too.
at
built in the
plants at
on the Columbia River
in
can be
electric
Grand
Washington
on the Colorado River. These
Dams have been
Tennessee River. They make
electricity for
the people of Tennessee, Mississippi and Alabama. also prevent floods of the
Tennessee River. 37
They
Rivers and Travel
Men
have sailed on
years. It
was the
rivers
easiest
way
and for
seas for thousands of
them
to travel.
So they
often settled along the shores of rivers and seas.
The first American settlements were on the Atlantic Ocean or on rivers that flowed into the Atlantic. As these settlements grew, they began to trade with each other
more and more. Settlements on the upper part could send their goods downstream on
rafts
of a river
and
flat-
The river current did the work. The rafts and flatboats were built for one trip only. They were cheap. But they were slower than ships. Many settlements along rivers could be reached by ships that safled across the ocean. Ocean ships could travel up the St. Lawrence as far as Montreal, Canada.
boats.
But ocean ships could not reach the settlements along
^iSSi
A f latboat
the Great Lakes.
Canal was
To reach
built. It
was
the Great Lakes, the Erie
finished in 1825. It connected
Lake Erie with the Hudson
River.
Ocean
ships
and Great
Lakes ships couldn't travel through the canal. Their goods had to be unloaded onto canal barges. So travel through the canal was slow.
Then
railroads
were
built. It
the goods of ocean ships canals
and
rivers
by
became cheaper
railroad. So, for
were not used
as
much
to
many
send
years,
for carrying
goods.
But now
rivers are
being used again. With the help of
dams, deep canals, and locks, rivers have been opened to large ships.
Now ships can use the Tennessee River even
during the dry season. The
ocean ships to travel
on
all
the
St.
Lawrence Seaway allows
way to Lake Superior. been made safer and
the Mississippi River has
Travel better.
ontreaf
UN^TED STATES Ocean ships now
travel to the Great
Lakes
Where People Live
New York City, Tokyo and London are the largest cities in the world. All of them are near rivers. All of
by ocean
ships.
too, are usually
m
them can be reached
Small
cities
and towns,
near rivers or the sea.
People built settlements on rivers for
'
¥'
\
many
reasons.
to get
away quickly
ger.
A
They wanted if
be able
to
they were in dan-
nearby river made a
fast
escape
possible.
They built their
settlements where they
could get food easily. They could catch fish
and oceans. They could hunt
in the rivers
animals in the woods along the shores. They could grow plants for food in the fertile soil of
They built could trade
the river valley. their settlements
easily.
where they
The barges and
boats
of a river joined one trading post with
another.
The
early settlers along the
River used the river in their living.
ikffiliFLC
Hudson
many ways
to earn
At Haverstraw, they used Hudson River clay to
make
bricks.
down
Ships sailed
the river from
New-
burgh and then up to the far North Atlantic
Ocean The
to catch whales.
rivers.
The
to
cut ice from the frozen
settlers
ice
went
keep food from Loggers cut
into people's iceboxes
spoiling.
down
near the
tall trees
upper Hudson. They floated them mills
to saw-
downstream.
At Troy, water that flowed into the
Hudson River was used to turn factory machinery. This helped make Troy a city of
many
factories.
Albany began It
was
as a post for fur traders.
in the center of Indian territory.
Furs were shipped from Albany
Hudson were
to
New
York
City,
down
the
where they
sold.
The
things people do to earn a living
keep changing. But most people near rivers or the
still
live
sea.
y.i
Water
for Plants
by animals and people. GrowThey get it from the soil through where there is plenty of rain, there
Plants are used as food
ing plants need water. their roots. In places is
always water in the
enough
rain, rivers
ervoirs are built
In places where there
soil.
is
not
can be used to water the land. Res-
where the
river valley
is
narrow and
deep.
Water keeps flowing out stream,
all
of the reservoir in a steady
year round. So even
when
it is
dry, the river
keeps flowing. Channels and ditches carry the water to fields
way
and orchards. Bringing water
is
to the land in this
called irrigation (ih-rig-GAY-shun).
and Grand Coulee also flood control
Dam
Hoover
are irrigation dams.
dams and
electric
Dam
They
are
power dams.
Water for People
Towns and live in
them.
cities
have
Some
cities
to get
water to the people
water of streams and rivers in
reservoirs.
Water
is
carried in pipes from the reservoirs to the towns cities for
New
then
and
people to use.
York City gets most of
in the Catskill skill
who
get their water by storing the
its
water from reservoirs
Mountains. Water from one of the Cat-
reservoirs travels 125 miles to
New
York City.
42
*
Los Angeles, California, gets
its
water from the Colo-
rado River, 300 miles away.
Keeping Water Clean
The people who them
live
near rivers do not always use
dump
wisely. Factories often
rivers.
Sometimes sewers empty
water of these
rivers
is
polluted (po-LUTE-ed). rivers.
Even
into the rivers.
no longer pure. It is
It
The
has become
not safe to bathe in these
the fish in a polluted river die.
People must learn that they
their wastes into the
how
to get rid of their wastes so
do not pollute the
rivers.
USOA
Dead
fish in a polluted
stream
Photograph
Deltas All the rivers of the world reach the sea sooner or
The
later.
may be an
sea
Or
inland salty lake.
it
may be
one of the oceans. The place where the river enters the sea
it
called the river's mouth.
is
A
river
sometimes drops the
carries at
rest of the
sand and
mouth. This happens where the sea
its
very quiet. The water of the Mediterranean Sea quiet.
soil
The water of the Gulf
of
Mexico
is
is
is
very
very quiet, too.
So a river that flows into the Mediterranean Sea or the Gulf of Mexico slows
drop
its
load of
at the river's
soil
mouth
down
very quickly. This makes
and sand. The sand and in the
Greek
letter "delta" looks like
and sand
Some
rivers
is
has been built on
Ganges River
Some no
rivers
delta. It
distance
deltas.
The
so large that the city of it.
The
in India
this layer
have no
deltas, too.
The Columbia River has down quickly at its mouth. So
deltas.
soil it carries
by the waves
delta of the
New Orleans
Nile River in Egypt and the
have very large
does not slow
the sand and
a triangle. So
called a delta (DELL-tuh).
have very large
Mississippi River
up
shape of a large triangle. The
of soil
is
soil pile
it
are spread out over a great
of the Pacific Ocean.
A river with a delta enters the sea through many channels.
Dried-out channels at the mouth of the Mississippi 44
I River
tell
us that
Po River in city of It is
its
Italy has
delta has
moved
moved. The delta of the
15 miles in 1,000 years.
The
Adria used to be a seaport at the mouth of the Po.
now
15 miles inland.
Delta of the Mississippi River
The Journey
Drop
of a
When you boil a pot of water,
Water
of
the heat from the stove
changes the water to water vapor or steam.
We say that
the water evaporates (ee-VAP-or-ates). River water evaporates, too.
As a
down
river flows
to the sea, the heat of
the sun changes some of the water to water vapor.
the vapor rises up into the
The
river
of the ocean.
water that reaches an ocean becomes part
The oceans cover most
of the earth. Great
amounts of water evaporate from the oceans,
When cooled. little
water vapor
The
rises
high up into the
drops of water or to bits of
little
heavy that they rain
too. air,
it
is
cooling changes the water vapor back to ice.
A
drops of water or bits of ice together times, the
Then
air.
a cloud. At
drops of water or bits of ice become so fall to
and
The away
the ground as rain or snow.
and melted snow may run
into the streams
lot of these little
make
rivers.
off the
land right
Or they may become ground
water which goes into the streams and rivers very slowly. Streams and rivers make their
way
to seas
and oceans.
Then the story begins all over again. The story of the journey of a drop of river water is called the water cycle (SY-kuU). The water cycle happens over and over again. So the story of the journey of a drop of river water a story without an end. 46
is
The Water cycle
WORD Bayou
LIST
(BYE-you) — A swampy lake formed when
a river
is
cut
a meander of
off.
Delta (DELL-tuh) the sand and
— Land
mud
built
up
at the
mouth
of a river
by
that the river drops there.
Erosion (ee-ROW-zhun)
— The wearing away of land by flowing
water.
Evaporation
(
ee-vap-or-AY-shun )
— Changing
a liquid,
like
water, into vapor or gas.
Flood plain (flud) — The level land in the broad valley of an old river, where the river drops sand and soil during floodtime. Generator (JEN-ur-ay-tor) Gravity
— The
—A
Horizontal (hah-rih-ZON-tuU) Irrigation
(
machine that makes
pull of the earth that
ih-rig-GAY-shun )
makes things
electricity.
fall.
— Level, like the top — Bringing water to
of a desk.
dry land
through pipes and ditches.
Levee (LEH-vee) — A wall the low land next to it.
of earth along a river that protects
— One of the turns in a winding river. (REZ-ur-vwar) — A lake in which water is stored. (TRIB-you-ter-ree) — A stream that empties into an-
Meander (mee-AN-dur) Reservoir
Tributary
other stream.
Turbine (TUR-bin) — A wheel that is turned when flowing water or a gas hits it. It is used to turn an electric generator. Vertical (VUR-ti-kuU)
— Standing
straight
up and down,
like a
tree.
Watershed
— The
land from which water drains into a
Weathering — The breaking up of rocks into air and water.
48
soil
river.
and stones by