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Unit 2 Lesson 6 Earthquakes
Florida Benchmarks
Copyright © Houghton Mifflin Harcourt Publishing Company
• SC.7.N.1.1 Define a problem from the seventh
grade curriculum, use appropriate reference
materials to support scientific understanding, plan
and carry out scientific investigations of various
types, such as systematic observations or
experiments, identify variables, collect and
organize data, interpret data in charts, tables, and
graphics, analyze information, make predictions,
and defend conclusions.
Unit 2 Lesson 6 Earthquakes
Florida Benchmarks
Copyright © Houghton Mifflin Harcourt Publishing Company
• SC.7.E.6.5 Explore the scientific theory of plate
tectonics by describing how the movement of
Earth’s crustal plates causes both slow and rapid
changes in Earth’s surface, including volcanic
eruptions, earthquakes, and mountain building.
• SC.7.E.6.7 Recognize that heat flow and
movement of material within Earth causes
earthquakes and volcanic eruptions, and creates
mountains and ocean basins.
Unit 2 Lesson 6 Earthquakes
Florida Benchmarks
Copyright © Houghton Mifflin Harcourt Publishing Company
• LA.7.4.2.2 The student will record information
(e.g., observations, notes, lists, charts, legends)
related to a topic, including visual aids to organize
and record information, as appropriate, and
attribute sources of information.
Let’s Focus
Copyright © Houghton Mifflin Harcourt Publishing Company
What is an earthquake?
• Earthquakes are ground movements that occur
when blocks of rock in Earth move suddenly and
release energy.
• The energy is released as seismic waves that
cause the ground to move.
Unit 2 Lesson 6 Earthquakes
What is an earthquake?
• The place within Earth where the first motion
occurs is called the focus.
• The place on Earth’s surface above the focus is
called the epicenter.
Copyright © Houghton Mifflin Harcourt Publishing Company
Unit 2 Lesson 6 Earthquakes
What causes earthquakes?
• Most earthquakes occur near a tectonic plate
boundary, which is where two or more tectonic
plates meet.
• The movement of tectonic plates breaks Earth’s
crust into a series of faults, which are breaks in
Earth’s crust along which blocks of rocks move.
• The release of energy that accompanies the
movement of rock along a fault is what causes an
earthquake.
Copyright © Houghton Mifflin Harcourt Publishing Company
Unit 2 Lesson 6 Earthquakes
What causes earthquakes?
• Stress causes deformation, which is the process
by which rock changes shape.
• As stress on rock increases, the energy stored in it
increases.
• When the stress is released, the rock sometimes
returns to its original shape.
Copyright © Houghton Mifflin Harcourt Publishing Company
Unit 2 Lesson 6 Earthquakes
What causes earthquakes?
• Deformation in which rock can spring back to its
original shape is called elastic deformation.
• The return of rock to its original shape after
elastic deformation is called elastic rebound.
Copyright © Houghton Mifflin Harcourt Publishing Company
Unit 2 Lesson 6 Earthquakes
Unstable Ground
Copyright © Houghton Mifflin Harcourt Publishing Company
Where do earthquakes happen?
• Most earthquakes happen at or near tectonic plate
boundaries.
• At tectonic plate boundaries, stress builds up from
tectonic plates colliding, separating, or grinding
past each other.
Unit 2 Lesson 6 Earthquakes
Where do earthquakes happen?
• At divergent boundaries, tension stress causes
normal faults to form. Earthquakes tend to be
shallow because the crust is thin.
Copyright © Houghton Mifflin Harcourt Publishing Company
Unit 2 Lesson 6 Earthquakes
Where do earthquakes happen?
• At convergent boundaries, rock is squeezed,
causing reverse faults to form. Earthquakes can
be very strong and deep.
Copyright © Houghton Mifflin Harcourt Publishing Company
Unit 2 Lesson 6 Earthquakes
Where do earthquakes happen?
• At transform boundaries, shear stress pushes
tectonic plates in opposite directions. Earthquakes
tend to be relatively shallow.
Copyright © Houghton Mifflin Harcourt Publishing Company
Unit 2 Lesson 6 Earthquakes
What are some effects of earthquakes?
• Most earthquakes do not cause damage, but some
strong earthquakes can cause major damage and
loss of life, especially in areas closest to the
epicenter.
• When the shaking of an earthquake is more than
structures can withstand, major destruction can
occur.
• Much of the injury and loss of life after an
earthquake is caused by structures that collapse.
Copyright © Houghton Mifflin Harcourt Publishing Company
Unit 2 Lesson 6 Earthquakes
What are some effects of earthquakes?
• An earthquake under the ocean can cause a
vertical movement of the sea floor that displaces
an enormous amount of water. This can generate
a tsunami.
• A tsunami is a series of extremely long waves that
can travel across the ocean at speeds of up to
800 km/h.
• As the waves reach the shoreline, the height of
the waves increases. The huge waves can cause
major destruction.
Copyright © Houghton Mifflin Harcourt Publishing Company
Unit 2 Lesson 6 Earthquakes
Unit 2 Lesson 6 Earthquakes
Killer Quake
Copyright © Houghton Mifflin Harcourt Publishing Company
• In 2004, an earthquake generated a tsunami that
wiped out half the population in Banda Aceh,
Indonesia.
• The tsunami traveled outward from the epicenter
in the Indian Ocean. Banda Aceh was very close to
the epicenter.
• The tsunami affected coastal areas around the
entire Indian Ocean, even reshaping many
coastlines in Asia.

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sc_7_e_6_5 earthquake (4).ppt

  • 1. Unit 2 Lesson 6 Earthquakes Florida Benchmarks Copyright © Houghton Mifflin Harcourt Publishing Company • SC.7.N.1.1 Define a problem from the seventh grade curriculum, use appropriate reference materials to support scientific understanding, plan and carry out scientific investigations of various types, such as systematic observations or experiments, identify variables, collect and organize data, interpret data in charts, tables, and graphics, analyze information, make predictions, and defend conclusions.
  • 2. Unit 2 Lesson 6 Earthquakes Florida Benchmarks Copyright © Houghton Mifflin Harcourt Publishing Company • SC.7.E.6.5 Explore the scientific theory of plate tectonics by describing how the movement of Earth’s crustal plates causes both slow and rapid changes in Earth’s surface, including volcanic eruptions, earthquakes, and mountain building. • SC.7.E.6.7 Recognize that heat flow and movement of material within Earth causes earthquakes and volcanic eruptions, and creates mountains and ocean basins.
  • 3. Unit 2 Lesson 6 Earthquakes Florida Benchmarks Copyright © Houghton Mifflin Harcourt Publishing Company • LA.7.4.2.2 The student will record information (e.g., observations, notes, lists, charts, legends) related to a topic, including visual aids to organize and record information, as appropriate, and attribute sources of information.
  • 4. Let’s Focus Copyright © Houghton Mifflin Harcourt Publishing Company What is an earthquake? • Earthquakes are ground movements that occur when blocks of rock in Earth move suddenly and release energy. • The energy is released as seismic waves that cause the ground to move. Unit 2 Lesson 6 Earthquakes
  • 5. What is an earthquake? • The place within Earth where the first motion occurs is called the focus. • The place on Earth’s surface above the focus is called the epicenter. Copyright © Houghton Mifflin Harcourt Publishing Company Unit 2 Lesson 6 Earthquakes
  • 6. What causes earthquakes? • Most earthquakes occur near a tectonic plate boundary, which is where two or more tectonic plates meet. • The movement of tectonic plates breaks Earth’s crust into a series of faults, which are breaks in Earth’s crust along which blocks of rocks move. • The release of energy that accompanies the movement of rock along a fault is what causes an earthquake. Copyright © Houghton Mifflin Harcourt Publishing Company Unit 2 Lesson 6 Earthquakes
  • 7. What causes earthquakes? • Stress causes deformation, which is the process by which rock changes shape. • As stress on rock increases, the energy stored in it increases. • When the stress is released, the rock sometimes returns to its original shape. Copyright © Houghton Mifflin Harcourt Publishing Company Unit 2 Lesson 6 Earthquakes
  • 8. What causes earthquakes? • Deformation in which rock can spring back to its original shape is called elastic deformation. • The return of rock to its original shape after elastic deformation is called elastic rebound. Copyright © Houghton Mifflin Harcourt Publishing Company Unit 2 Lesson 6 Earthquakes
  • 9. Unstable Ground Copyright © Houghton Mifflin Harcourt Publishing Company Where do earthquakes happen? • Most earthquakes happen at or near tectonic plate boundaries. • At tectonic plate boundaries, stress builds up from tectonic plates colliding, separating, or grinding past each other. Unit 2 Lesson 6 Earthquakes
  • 10. Where do earthquakes happen? • At divergent boundaries, tension stress causes normal faults to form. Earthquakes tend to be shallow because the crust is thin. Copyright © Houghton Mifflin Harcourt Publishing Company Unit 2 Lesson 6 Earthquakes
  • 11. Where do earthquakes happen? • At convergent boundaries, rock is squeezed, causing reverse faults to form. Earthquakes can be very strong and deep. Copyright © Houghton Mifflin Harcourt Publishing Company Unit 2 Lesson 6 Earthquakes
  • 12. Where do earthquakes happen? • At transform boundaries, shear stress pushes tectonic plates in opposite directions. Earthquakes tend to be relatively shallow. Copyright © Houghton Mifflin Harcourt Publishing Company Unit 2 Lesson 6 Earthquakes
  • 13. What are some effects of earthquakes? • Most earthquakes do not cause damage, but some strong earthquakes can cause major damage and loss of life, especially in areas closest to the epicenter. • When the shaking of an earthquake is more than structures can withstand, major destruction can occur. • Much of the injury and loss of life after an earthquake is caused by structures that collapse. Copyright © Houghton Mifflin Harcourt Publishing Company Unit 2 Lesson 6 Earthquakes
  • 14. What are some effects of earthquakes? • An earthquake under the ocean can cause a vertical movement of the sea floor that displaces an enormous amount of water. This can generate a tsunami. • A tsunami is a series of extremely long waves that can travel across the ocean at speeds of up to 800 km/h. • As the waves reach the shoreline, the height of the waves increases. The huge waves can cause major destruction. Copyright © Houghton Mifflin Harcourt Publishing Company Unit 2 Lesson 6 Earthquakes
  • 15. Unit 2 Lesson 6 Earthquakes Killer Quake Copyright © Houghton Mifflin Harcourt Publishing Company • In 2004, an earthquake generated a tsunami that wiped out half the population in Banda Aceh, Indonesia. • The tsunami traveled outward from the epicenter in the Indian Ocean. Banda Aceh was very close to the epicenter. • The tsunami affected coastal areas around the entire Indian Ocean, even reshaping many coastlines in Asia.

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