Title: Changing Earth
1Table of Contents
- Changing Earths Surface
- Water Erosion
- The Force of Moving Water
- Glaciers
- Waves
- Wind
2Wearing Down and Building Up
- Changing Earths Surface
- Weathering, erosion, and deposition act together
in a cycle that wears down and builds up Earths
surface.
3Mass Movement
- Changing Earths Surface
- The different types of mass movement include
landslides, mudflows, slump, and creep.
4Mass Movement Activity
- Changing Earths Surface
- Click the Active Art button to open a browser
window and access Active Art about mass movement.
5Comparing and Contrasting
- Changing Earths Surface
- As you read, compare and contrast the different
types of mass movement by completing a table like
the one below.
Mass Movement
Type of Mass Movement
Speed
Slope
Landslide
rapid
steep
Mudflow
rapid
gentle to steep
Slump
rapid
steep
Creep
slow
gentle to steep
6Data Sharing Lab
- Click the PHSchool.com button for an activity
about sharing data for the Skills Lab Sand Hills.
7End of SectionChanging Earths Surface
8Runoff and Erosion
- Water Erosion
- Precipitation over the United States averages
about 75 cm per year. About 22.5 cm becomes
runoff. Generally, more runoff means more
erosion.
9Runoff and Erosion
- Water Erosion
- Water flowing across the land runs together to
form rills, gullies, and streams.
10Erosion by Rivers
- Water Erosion
- A waterfall forms where a flat layer of tough
rock lies over a layer of softer rock that erodes
easily. When the softer rock erodes, pieces of
the harder rock above break off, creating the
waterfalls sharp drop.
11Erosion by Rivers
- Water Erosion
- Erosion often forms meanders and oxbow lakes
where a river winds across its floodplain.
12Deposits by Rivers
- Water Erosion
- Deposition creates landforms such as alluvial
fans and deltas.
13The Course of a River
- Water Erosion
- The slope and size of a river, as well as the
sediment it carries, determine how a river shapes
the land.
14Groundwater Erosion
- Water Erosion
- Karst topography is found in many parts of the
United States where the bedrock is made up of
thick layers of limestone.
15Groundwater Erosion
- Water Erosion
- Chemical weathering of limestone and groundwater
erosion can create a limestone cave.
16Previewing Visuals
- Water Erosion
- Before you read, preview Figure 10. Then write
two questions you have about the illustration in
a graphic organizer like the one below. As you
read, answer your questions.
The Course of a River
Q. What features does a river produce by erosion?
A. V-shaped valley, bluffs
Q. What feature does a river produce by
deposition?
A. Delta
17More on Floods
- Water Erosion
- Click the Planet Diary button for an activity
about floods.
18End of SectionWater Erosion
19How Water Erodes
- The Force of Moving Water
- Most sediment washes or falls into a river as a
result of mass movement and runoff. Other
sediment erodes from the bottom or sides of the
river. Streams carry sediment in several ways, as
shown in the diagram.
20Erosion and Sediment Load
- The Force of Moving Water
- A rivers slope is usually greatest near the
rivers source. As a river approaches its mouth,
its slope lessens.
21Sediment on the Move
- The Force of Moving Water
- The speed, or velocity, of a stream affects the
size of the sediment particles the stream can
carry. Study the graph, then answer the following
questions.
22Sediment on the Move
- The Force of Moving Water
- Reading Graphs
- What variable is shown on the x-axis of the graph?
23Sediment on the Move
- The Force of Moving Water
- Reading Graphs
- What variable is shown on the y-axis of the graph?
- Diameter of sediment particles
24Sediment on the Move
- The Force of Moving Water
- Interpreting Data
- What is the speed at which a stream can move
coarse sand? Small pebbles? Large boulders?
- About 50 cm/sec about 90 cm/sec about 800 cm/sec
25Sediment on the Move
- The Force of Moving Water
- Predicting
- A streams speed increases to about 600 cm per
second during a flood. What are the largest
particles the stream can move?
26Sediment on the Move
- The Force of Moving Water
- Developing Hypotheses
- Write a hypothesis that states the relationship
between the speed of a stream and the size of
sediment particles it can move.
- The faster the speed of the flowing water, the
larger the particles the stream is able to move.
27Erosion and Sediment Load
- The Force of Moving Water
- A river erodes sediment from its banks on the
outside curve and deposits sediment on the inside
curve.
28Building Vocabulary
- The Force of Moving Water
- A definition states the meaning of a word or
phrase by telling about its most important
feature or function. Carefully read the
definition of each Key Term and also read the
neighboring sentences. Then write a definition of
each Key Term in your own words.
Key Terms
Examples
energy
Energy is the ability to do work or cause change.
The amount of sediment that a river carries is
its load.
Friction is the force that opposes the motion of
one surface as it moves across another surface.
potential energy
Potential energy is the energy that is stored and
waiting to be used later.
Instead of moving downstream, the water moves
ever which way in a type of movement called
turbulence.
kinetic energy
Kinetic energy is the energy an object has due to
its motion.
abrasion
Abrasion is the wearing away of rock by a
grinding action.
29More on River Erosion
- The Force of Moving Water
- Click the PHSchool.com button for an
activityabout river erosion.
30End of SectionThe Force of Moving Water
31How Glaciers Form and Move
- Glaciers
- A continental glacier is a glacier that covers
much of a continent or large island.
32How Glaciers Form and Move
- Glaciers
- During the last ice age, a continental glacier
covered most of northern North America.
33How Glaciers Shape the Land
- Glaciers
- As a glacier moves, plucking breaks pieces of
bedrock from the ground.
34How Glaciers Shape the Land
- Glaciers
- Erosion by glaciers can carve a mountain peak
into a sharp horn and grind out a V-shaped valley
to form a U-shaped valley.
35How Glaciers Shape the Land
- Glaciers
- As glaciers advance and retreat, they sculpt the
landscape by erosion and deposition.
36Asking Questions
- Glaciers
- Before you read, preview the red headings. In a
graphic organizer like the one below, ask a what,
how, or where question for each heading. As you
read, write answers to your questions.
Question
Answer
What kinds of glaciers are there?
Valley glaciers and continental glaciers
How do glaciers shape the land?
By erosion and deposition
37Links on Glaciers
- Glaciers
- Click the SciLinks button for links on glaciers.
38End of SectionGlaciers
39Erosion by Waves
- Waves
- Waves shape the coast through erosion by breaking
down rock and transporting sand and other
sediment.
40Erosion by Waves
- Waves
- Erosion and deposition create a variety of
features along a coast.
41Deposits by Waves
- Waves
- Waves shape a coast when they deposit sediment,
forming coastal features such as beaches, spits,
and barrier beaches.
42Identifying Main Ideas
- Waves
- As you read the section Erosion by Waves, write
the main idea in a graphic organizer like the one
below. Then write three supporting details that
further explain the main idea.
Main Idea
Waves cause erosion by impact and by abrasion.
Detail
Detail
Detail
Energy in waves breaks apart rocks.
Sediment wears away rock.
Landforms are created.
43Waves
- Waves
- Click the Video button to watch a movie about
waves.
44Links on Waves
- Waves
- Click the SciLinks button for links on waves.
45End of SectionWaves
46How Wind Causes Erosion
- Wind
- Wind erosion moves sediment particles of
different sizes in the three ways shown below.
47Wind Deposition
- Wind
- Wind erosion and deposition may form sand dunes
and loess deposits.
48Sequencing
- Wind
- As you read, make a flowchart like the one below
that shows the process of wind erosion and
deposition. Write each step of the process in a
separate box in the flowchart in the order in
which it occurs.
Wind Erosion
Wind picks up smallest particles of sediment.
Fine particles are carried through the air.
Medium-sized particles skip and bounce.
Larger particles slide or roll.
49End of SectionWind
50Graphic Organizer
Stream Formation
Raindrops strike ground.
Runoff forms.
Rills form.
Gullies form.
Gullies join together.
Stream forms.
51End of SectionGraphic Organizer