Title: Earth’s Extremes: Glaciers and Deserts Description: Explore the powerful forces shaping Earth’s surface in this exciting slideshow about glaciers and deserts. Learn how icy giants slowly carve out valleys and how winds sculpt stunning desert landscapes. Through vivid images and simple explanations, discover the processes of erosion, deposition, and climate impact in two of Earth’s most extreme environments. This presentation helps students understand the surprising similarities and key differences between frozen and arid ecosystems. This slideshow takes you on a journey through two of Earth’s most dramatic landscapes: glaciers and deserts. Discover how glaciers grind down mountains, transport massive amounts of rock, and shape U-shaped valleys, while deserts, shaped by wind and minimal rainfall, form dunes, mesas, and canyons. Learn how both environments reveal clues about Earth’s climate, water cycles, and geologic history. Perfect for classrooms or anyone curious about Earth science. This comprehensive slideshow explores the contrasting but equally dynamic geomorphic systems of glaciers and deserts. Examine the mechanisms of glacial erosion (plucking, abrasion), the formation of features like moraines and glacial troughs, and the role of aeolian processes in desert environments. Case studies include the Sahara Desert, the Atacama, and the Antarctic ice sheet. This presentation also touches on climate influences, past glaciations, and desertification trends. Ideal for advanced Earth science courses.

1. Prentice Hall
EARTH SCIENCE
EARTH SCIENCE
Tarbuck Lutgens
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2. Chapter
1
1
Introduction to
Earth Science

3. Overview of Earth Science
1.1 What Is Earth Science?
 Encompasses all sciences that seek
to understand
• Earth
• Earth's neighbors in space

4. Overview of Earth Science
 Earth science includes
4. astronomy, the study of the universe
3. meteorology, the study of the atmosphere
and the processes that produce weather
1. geology, the study of Earth
2. oceanography, the study of the ocean
1.1 What Is Earth Science?

5. Formation of Earth
• The solar system evolved from an enormous
rotating cloud called the solar nebula.
 Most researchers conclude that Earth
and the other planets formed at
essentially the same time.
 Nebular Hypothesis
1.1 What Is Earth Science?

6. Formation of Earth
• The nebula was composed mostly of
hydrogen and helium.
 Nebular Hypothesis
1.1 What Is Earth Science?
• About 5 billion years ago, the nebula began
to contract.
• It assumed a flat, disk shape with the
protosun (pre-Sun) at the center.

7. Formation of Earth
• Inner planets begin to form from metallic and
rocky clumps.
 Nebular Hypothesis
1.1 What Is Earth Science?
• Larger outer planets began forming from
fragments with a high percentage of ices.

8. The Nebular Hypothesis
A
C
D
E
B

9. Formation of Earth
 Layers Form on Earth
1.1 What Is Earth Science?
• As Earth formed, the decay of radioactive
elements and heat from high-velocity impacts
caused the temperature to increase.
• Lighter rocky components floated outward,
toward the surface.
• Gaseous material escaped from Earth’s interior
to produce the primitive atmosphere.

10. Earth's Major Spheres
1.2 A View of Earth
1. Hydrosphere
• Ocean is the most prominent feature of the
hydrosphere.
- Is nearly 71% of Earth's surface
- Holds about 97% of Earth's water
• Also includes fresh water found in streams,
lakes, and glaciers, as well as that found
underground

11. Earth's Major Spheres
1.2 A View of Earth
2. Atmosphere
• Thin, tenuous blanket of air
• One half lies below 5.6 kilometers (3.5 miles)
3. Biosphere
• Includes all life
• Concentrated near the surface in a zone that
extends from the ocean floor upward for
several kilometers into the atmosphere

12. Earth's Major Spheres
1.2 A View of Earth
4. Geosphere
• Based on compositional differences, it
consists of the crust, mantle, and core.
- Crust—the thin, rocky outer layer of Earth.
- Mantle—the 2890-kilometer-thick layer of
Earth located below the crust.
- Core—the innermost layer of Earth, located
beneath the mantle.

13. Earth’s Layered Structure

14. Plate Tectonics
1.2 A View of Earth
 Plate tectonics is the theory that
proposes that Earth’s outer shell
consists of individual plates that interact
in various ways and thereby produce
earthquakes, volcanoes, mountains, and
Earth’s crust itself.

15. Determining Location
1.3 Representing Earth’s Surface
Latitude and longitude are lines on the
globe that are used to determine
location.
• Latitude is distance north or south of the
equator, measured in degrees.
• Longitude is distance east or west of the
prime meridian, measured in degrees.

16. Maps and Mapping
1.3 Representing Earth’s Surface
 No matter what kind of map is made,
some portion of the surface will always
look either too small, too big, or out of
place. Mapmakers have, however, found
ways to limit the distortion of shape, size,
distance and direction.

17. Topographic Maps
1.3 Representing Earth’s Surface
 Topographic maps represent Earth’s
surface in three dimensions; they show
elevation, distance directions, and slope
angles.
• Contour lines are lines on a topographic map
that indicate an elevation.
• Contour interval is the distance in elevation
between adjacent contour lines.

18. What Is a System?
1.4 Earth System Science
 Closed systems are self contained
(e.g., an automobile cooling system).
 Open systems allow both energy and matter
to flow in and out of the system
(e.g., a river system).
 A system is any size group of interacting
parts that form a complex whole.

19. Earth as a System
1.4 Earth System Science
 Earth is a dynamic body with many
separate but highly interacting parts
or spheres.
 Earth system science studies Earth
as a system that is composed of
numerous parts, or subsystems.

20. Earth as a System
1.4 Earth System Science
 Sources of Energy
• Sun—drives external processes such as
weather, ocean circulation and erosional
processes
• Earth’s interior—drives internal
processes including volcanoes,
earthquakes and mountain building

21. Earth as a System
1.4 Earth System Science
 Humans are part of the Earth system.
 Consists of a nearly endless array of
subsystems (e.g., hydrologic cycle)

22. People and the Environment
1.4 Earth System Science
 Environment
• Surrounds and influences organisms
• Physical environment encompasses water,
air, soil, and rock
• The term environmental is usually reserved for
those aspects that focus on the relationships
between people and the natural environment.

23. People and the Environment
1.4 Earth System Science
 Resources
• Include water, soil, minerals, and energy
• Two broad categories
2. Nonrenewable—cannot be replenished in
the near future (e.g., metals, fuels)
1. Renewable—can be replenished (e.g.,
plants, energy from water and wind)

24. People and the Environment
1.4 Earth System Science
 Population
• Population of the planet is growing rapidly
• Use of minerals/energy has climbed more
rapidly than the overall growth of population

25. Growth of World Population

26. Environmental Problems
1.4 Earth System Science
 Caused by people and societies
• Urban air pollution
• Acid rain
 Caused by natural hazards
• Landslides
• Ozone depletion
• Global warming
• Earthquakes
 Local, regional, and global

27. Science
1.5 What Is Scientific Inquiry?
 Science assumes the natural world is
• consistent
• predictable
 Goals of science are
• to use the knowledge to predict
• to discover patterns in nature

28. Hypothesis and Theory
1.5 What Is Scientific Inquiry?
 An idea can become a
• hypothesis—tentative or untested explanation
• theory—tested, confirmed, supported hypothesis
 Scientific Method
• Formulate hypotheses
• Gather facts through observation
• Test hypotheses to formulate theories

29. Science Methods
1.5 What Is Scientific Inquiry?
 Scientific knowledge is gained through
• following systematic steps
1. Collecting facts
• theories that withstand examination
• totally unexpected occurrences
2. Developing a hypothesis
3. Conducting experiments
4. Reexamining the hypothesis and accepting,
modifying, or rejecting it