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
Published in 1994
This report illustrates how two organisms, a trilobite and a nautiloid, became fossils. The report is intended to help students and others visualize the size and shape of a trilobite and a nautiloid, the environment in which they lived, and the circumstances of their fossilization and subsequent...
Grade Level   3 4 5 6 7 8 9 10 11 12
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3
Chapter 5 focuses on Prehistoric Earth, geologic time, and early lifeforms on this planet.
Grade Level   K 1 2 3 4 5 6 7 8 9 10 11 12
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4
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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5
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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6
This interactive lesson from Annenberg Learner takes you through different time periods of major plate tectonic movement, from Pangea to present day.
Grade Level   9 10 11 12
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7
This activity uses the Earthquake Machine, a mechanical model that illustrates the earthquake cycle, as a tool to investigate the behavior of fault systems. In the activity groups of students are presented with a claim about earthquakes. Using the Earthquake Machine, students design an investigation...
Grade Level   5 6 7 8 9 10 11 12
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8
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
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9
"This activity asks """"deep questions"""" about sedimentary structures to help pupils to visualize the environment in which they formed."
Grade Level   9 10 11 12
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10
"Students will make a paper model illustrating the concept of sea-floor spreading and the development of symmetrical magnetic """"stripes"""" on either side of a mid- ocean spreading center."
Grade Level   5 6 7 8 9 10 11 12
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11
"This hands-on activity requires students to """"visit"""" different K-T boundary sites, evaluate the evidence at each site, find these sites on a map, and predict where the crater is located. It tests a diverse set of skills, including mapping, mathematical scaling, and interpretation of mixed...
Grade Level   6 7 8 9 10 11 12
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