1
In this lesson, students will create three-dimensional (3-D) blocks out of paper to learn about the types of faulting that occur at the Earth’s surface and its interior, and explain how earthquakes are generated by fault movement. Step-by-step directions will provide students with the necessary...
Grade Level   K 1 2 3 4 5 6 7 8 9 10 11 12
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2
Chapter 1 focuses on Plate Tectonics looking at the Earth's layers, Earth's evolution, and plate movement. Lessons included in this chapter: Earth's layers, Pangea to present, How Earth's Plates Move.
Grade Level   K 1 2 3 4 5 6 7 8 9 10 11 12
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3
Students will be able to discuss how different magnitudes of earthquakes affect structures differently by simulating how buildings become damaged in an earthquake.
Grade Level   4 5 6 7 8
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4
In this lesson, students examine seismic evidence to determine a) Earth must have a layered internal structure and, b) estimate the size of Earth’s core. Using an inquiry approach, students are divided into two teams (theoreticians and seismologists) to test the simplest hypothesis for what is...
Grade Level   K 1 2 3 4 5 6 7 8 9 10 11 12
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5
How do geologists understand the Earth’s history? In part, they measure the age of rocks and other natural materials by dating techniques. They can date rocks by gauging the amount of decay of radioactive elements. The time necessary for half of any given amount of one element (the “parent...
Grade Level   5 6 7 8 9
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6
Geologists take advantage of decay of natural radioactive elements to determine the age of rocks, which can help us understand earth history. One example of this dating method is using volcanic ash layers to help determine the age of ash-bearing horizons in ice cores. Ice cores provide important...
Grade Level   4 5 6 7 8 9 10 11 12
Classroom Activities Curricula and Instruction
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