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Reshaping the land

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Photo Credits: Cover: Gary Braasch/Corbis; p. 2: N. A. Callow/ Photo Researchers,
Inc.; p. 3: Mark Newman/ Photo Researchers, Inc.; p. 4: Earth Satellite Corporation/
Photo Researchers, Inc.; p. 5: George Ranalli/ Photo Researchers, Inc.; p. 6: Jeff
Rotman/ Photo Reseachers, Inc.; p. 7: Mickey Gibson/ Animals Animals/ Earth Scenes;
p. 8: Harcourt; p. 9: David Parker/ Photo Researchers, Inc.; p. 10: C.C. Lockwood/
Animals Animals/ Earth Scenes; p. 11: Bryan & Cherry Alexander/ Photo Researchers,
Inc.; p. 12: Larry L. Miller/ Photo Researchers, Inc.; p. 13: Alfred Pasieska/ Photo
Researchers, Inc.; p. 14: Eye of Science/ Photo Researchers, Inc.; p. 15: George H. H.
Huey/ Corbis.

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ISBN-13: 978-0-15-352352-6
ISBN-10: 0-15-352352-2
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Moving Water Shapes Earth .................................. 2
Moving Ice Shapes Earth ....................................... 4
Wind Shapes Earth.............................................. 6
Weathering Shapes ............................................. 8
Freezing and Thawing Shapes Earth ......................... 10
Glossary........................................................... 12

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Moving Water Shapes Earth
Rivers change the surface of Earth. A river shapes the
land around it. Valleys that are narrow and steep are made

by quickly flowing water. The water wears away the soil
and rock.
Valleys with older rivers are wider and less steep than
newer rivers. The floors of the older rivers are flatter.
Rivers carry soil and rock. The dropping of bits of rock
and soil by a river as it flows is called deposition. Deltas at
the ends of rivers and plains along riverbanks are formed
by deposition.
Landforms are also changed by ocean waves that hit cliffs
along the shore. Waves move sand from one part of the
coastline to another.

The Mississippi
Delta was formed
by deposition that
took place over
years and years.

2

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Water shapes the land by causing erosion. In the process
of erosion, materials carried by moving water are dropped in
new locations. For example, a flood from a hurricane might
erode barrier islands, or small islands along a shore. Next,
the floodwater might carry the sand from those islands and

deposit it in a river delta. Ocean waves can eat away at rock
formations along the shore. In time, the pieces of rock that
were worn away can be deposited on a nearby beach.
CAUSE AND EFFECT How are valleys formed?

The foundation of this house
has been eroded. Soon, this
house and the ones beyond it
may fall into the ocean below
them.

3

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Moving Ice
Shapes Earth
In cold climates where snow piles
up from one year to another, the
snow turns to ice. Sometimes the ice
begins to move. It becomes a glacier,
or a large moving block of ice. Alpine,
or mountain, glaciers cause valleys
to widen.
Glaciers also move in large sheets.
Sheets of ice covered much of Earth
thousands of years ago. They moved

over the land and changed its surface.

The ice sheet in
Antarctica is over
13 million square
kilometers (7,800,000
square mi). Its thickest
point is over 4.5
kilometers (2.7 mi).
The Antarctic ice sheet
holds 70 percent
of the fresh water
on Earth.

Alpine glaciers, ice
sheets, and other
forms of ice can be
found in Antarctica.

4

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The Great Lakes are among the landforms the glaciers
carved. During the Ice Ages, glaciers scraped deeply into the
land where the lakes are now. When the glaciers melted, the
water was left behind. In other places, the glaciers left

behind hills of the rocks, sand, and clay that had been
trapped in the ice.
DRAW CONCLUSIONS How can ice scrape something as
hard as rock?

These rock
formations are called
glacial grooves. They
formed when the
land that is now Ohio
was under glaciers.

5

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Wind Shapes Earth
The action of wind has formed many interesting
landforms. In places such as the deserts of the southwest,
the rock is somewhat soft. The wind picks up pieces of sand
and soil from the dry ground and blows it against the rocks.
Over many years, the wind shapes the rocks into forms that
look like arches, tables, and columns.
Wind also shapes large areas of inland dunes in deserts,
such as those in Africa. There, the sand piles up like
mountains in dunes that shift from year to year.
Over thousands of years,

wind and rain have
shaped this formation in
Monument Valley, Utah.

6

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As the wind blows across a
beach, the plants on the
dunes slow it down. The sand
falls to the ground, adding to
the size of the dunes..

These tall dunes in Arizona
were shaped by the wind.

In some instances, wind can be a helpful force in shaping
land. For example, winds shape beach sand into dunes.
Beach dunes form where plants and rocks slow down the
ocean breezes, causing the sand to drop to the ground.
However, wind can be a harmful force, too. In the
1930s, the North American prairie had a number of
droughts. Farming practices were also poor. As a result,
millions of acres of soil were blown away by the wind.
MAIN IDEA AND DETAILS How does sand being carried
by wind get back to the ground?

7

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Weathering Shapes Earth
1 as a
ain
rials at
this

his
m
e class.
n the

Earth’s landforms are always changing. One cause of
change is weathering, or the process of breaking rock into
silt, sand, clay, and other tiny particles. Water cuts canyons
and valleys. It crashes in waves against beaches. In rivers, it
flows across rocks and stones and makes them smooth. Even
the roots of plants that grow into rock help weather the
rock. These are examples of mechanical weathering, or the
breaking up of rock by physical processes. With mechanical
weathering, rocks may break, but they keep their properties.
The roots of plants
can cause mechanical
weathering of rocks.


--------

neath

as
also
rust
the
e, and
er
ep.
e
8

Ground

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These river rocks are
weathered. As water
flowed over them,
they tumbled against
other stones and lost
their rough edges.

Chemical weathering

has given this rock’s
surface a brown
color. Iron in the rock
is rusting and is
breaking down the
outer layer.

Another kind of weathering is chemical weathering, in
which rocks break up, but their properties are changed by
chemicals. An example of this is acid rain, which dissolves
some kinds of rock. Another example is rusting in ironbearing rocks.
Some kinds of weathering are very helpful. It is necessary
for bedrock, or solid rock below the soil, to weather. In this
way, new soil is formed.
COMPARE AND CONTRAST How is mechanical
weathering different from chemical weathering? How is
it the same?
9

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Freezing and
Thawing Shape Earth
Water is a powerful thing. What is it about the
freezing and thawing of water that is so powerful?
Water expands when it freezes. When it rains on
rocks, the rain seeps into the tiny cracks in the rocks. If the

rain freezes, the water inside the rock freezes too. As the

When ice freezes in
rock, the ice expands
and cracks it.

10

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water freezes, it expands. This forces the cracks apart a little
more than they already were. When the ice thaws, the
cracks remain. When it rains again, the process repeats–until
finally the rock splits.
Frozen water is also hard, and glaciers are very heavy.
Because of this, the rocks and pebbles trapped below the ice
have great force. This causes the glacier to act like
sandpaper, scraping the ground below them.
CAUSE AND EFFECT How can rainwater cause rocks to
crack?

Summary
Powerful forces cause Earth’s landforms to change.
Moving water forms valleys and canyons and cuts
deep riverbeds. Moving ice in glaciers cuts lakebeds,
valleys, and grooves. The wind also shapes Earth by
carving soft rock into shapes, and it builds beaches

and dunes. Weathering is the breaking down of rock
into particles. The different kinds of weathering are
mechanical weathering and chemical weathering.
Freezing and thawing help rocks weather. Water
freezes in the cracks of rocks and expands the cracks.

11

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Glossary
chemical weathering (kem•ih•kuhl weth•er•ing) Process in
which rocks break up, and their properties are also changed
by chemicals (8)
deposition (dep•ih•ZISH•uhn) The dropping of bits of rock
and soil by a river as it flows (10)
glacier (GLAY•sher) A large, moving block of ice (3, 11)
mechanical weathering (muh•kan•ih•kuhl weth•er•ing)
the breaking up of rock by physical processes (8)

12

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Think and Write
1. How does weathering help make new soil?
2. DRAW CONCLUSIONS Look at pages 2–5 and
8–11 as a whole. What can you conclude is one of
the main things that shapes Earth?
3. CAUSE AND EFFECT What happens to eroded
materials at the mouth of the Mississippi River?
Why does this happen?
4. Expository Writing Try to describe fossil
footprints to a young child. Compare different kinds
of footprints. Explain to the child what we can learn
from fossil footprints.

Hands-On Activity
Make a flip book of one of the changes described in this
Reader. Try to show the change or process from beginning
to end. Present your flip book to the class. See if others can
describe what is happening in the pictures.

School-Home Connection
Find some loose soil or rocks that could easily be changed
by moving water. Take a photograph or draw a picture of
the soil. Wait a few weeks. Draw another picture. Discuss the
changes you notice with people in your family.

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