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Earth’s Change: Rapid Processes

Lesson Plan

Earth’s Change: Rapid Processes

Objectives

In this lesson, students will learn about tectonic plate movements and how we use this theory to hypothesize what Earth’s past geological features and biological inhabitants were like. Students will:

  • relate changes on Earth with tectonic plate movements.

  • use fossil evidence as evidence of tectonic plate movement.

  • hypothesize what Earth looked like millions of years ago.

Essential Questions

Vocabulary

  • Fossil: The remains of an animal or plant preserved from an earlier era inside a rock or a geological deposit, often as an impression or in a petrified state.

  • Mesozoic Era: The era of geologic time that includes the Triassic, Jurassic, and Cretaceous periods.

  • Pangaea: A supercontinent that existed during the Mesozoic Era that included most of Earth’s present-day continents.

  • Plate Tectonics: A theory that explains movements of continents and changes in Earth’s crust caused by internal forces within the planet.

  • Glossopteris: A fern found on the southern continents.

  • Cynognathus: A land reptile found in South America and Africa.

  • Lystrosaurus: A land reptile found in Africa, Antarctica, and India.

  • Mesosaurus: A freshwater swimming reptile found in Africa and South America.

Duration

60 minutes/ two class periods

Prerequisite Skills

Prerequisite Skills haven't been entered into the lesson plan.

Materials

Related Unit and Lesson Plans

Related Materials & Resources

The possible inclusion of commercial websites below is not an implied endorsement of their products, which are not free, and are not required for this lesson plan.

Formative Assessment

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    • Students will be assessed on their general knowledge of plate separation and fault lines which caused the separation of Gondwanaland through their project presentations and whole-group discussion.

    • Students will be assessed through whole group discussion on fossil location and why some fossils are on many different continents.

    • Students will be assessed on whether Du Toit’s theory is true or false, based on the evidence they give in their project and presentation.

    • Students will be assessed on their knowledge of maps and locations, as well as on their map presentation to the class. They will also be assessed on their presentation voice and clarity of speaking to the class.

Suggested Instructional Supports

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    Active Engagement, Modeling, Explicit Instruction
    W:

    Students will learn about Earth’s surface and how the continents once looked. They will learn about Pangaea and Gondwanaland and how they looked. Students will become familiar with fossils and how similar fossils ended up in different continents.

    H:

    Students will make assumptions about what Earth used to look like before it started separating. They will make predictions and take part in a class discussion.

    E:

    Students will label the map of Earth indicating where fossils were found, and then piece together the seven continents to make a Pangaea or a Gondwanaland.

    R:

    Students will have a discussion and share their predictions and explain why fossils were found in specific locations and why the Pangaea or Gondwanaland looked the way it did.

    E:

    Students will then take formative assessment and answer questions pertaining to the classroom activities.

    T:

    This lesson is designed to give student hands-on experience by creating their own Pangaea or Gondwanaland and to allow for critical thinking skills when creating hypotheses on how Earth has changed. All learners at all levels will be drawn into the lesson because it provides many different teaching strategies.

    O:

    You will begin the lesson by pre-assessing what students already know about the Earth’s surface and movement of the continents. Students move to independent learning by creating the fossil maps and their Pangaea or Gondwanaland. They will use oral speaking skills and writing skills to present their findings that will lead to whole group discussion to come up with a conclusion on why Earth changed and why fossils ended up where they did.

Instructional Procedures

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    Day 1

    Begin the lesson by showing the class a standard physical map of the world. Tell students to look closely at the continents. Ask, “Do you think the continents always looked as they do on the map, or did they change shape or location throughout Earth’s history?” Write their ideas on a large sheet of paper or on the board.

    Tell students, “In early 1915, the German scientist Alfred Wegener developed a theory that the continents once formed a giant supercontinent that he called ‘Pangaea.’ ” See the map of Pangaea (S-8-6-1_Pangaea.doc).

    He speculated that Earth took this form about 245 million years ago, during the Triassic period of the Mesozoic Era. (The Mesozoic is the era in which dinosaurs lived.) A few years after Wegener proposed his theory, South African geologist Alexander Du Toit further theorized that Pangaea divided into two supercontinents 205 million years ago. Du Toit called the northern supercontinent Laurasia and the southern one Gondwanaland. The scientists used many kinds of evidence to advance their theories. They found similar fossil remains of plants and animals on different present-day continents. The scientists hypothesized that the continents were once connected.”

    Ask students, “If you follow steps similar to those of Wegener and Du Toit, will you see fossil evidence that supports the theory that one supercontinent was divided?” Hand out copies of the Prehistoric Land Masses activity sheet (S-8-6-1_Prehistoric Land Masses.pdf). Tell students they will focus on Gondwanaland, the supercontinent that includes South America, Antarctica, Australia, Africa, Madagascar, and India.

    Tell students that they will map the locations of four different fossils:

    • Glossopteris: A fern found on the southern continents

    • Cynognathus: A land reptile found in South America and Africa.

    • Lystrosaurus: A land reptile found in Africa, Antarctica, and India.

    • Mesosaurus: A freshwater swimming reptile found in Africa and South America.

    Students should mark these locations on the sheet, using the map key code.

    Tell students to cut out the continent shapes and try to piece them together as Gondwanaland. Ask them to think about how the different shapes fit together. For homework, have students paste their finished version of Gondwanaland on the Prehistoric Land Mass activity sheet.

    Day 2
    During the next class period, have students share their versions of Gondwanaland.
    Are most constructions similar?” Show students a picture of what scientists believe
    Gondwanaland looked like (S-8-6-1_Gondwanaland.doc).

    Ask students, “Knowing where the fossil remains have been found, does this evidence support Wegener and Du Toit’s theory? Do you think it is sufficient evidence? What other information would be helpful?” Tell students that over the past century, scientists have continued to find evidence supporting this theory.

    Extension:
    For the whole class, common Pennsylvania fossils can be reviewed through group discussion. Questions on why certain types of fossils may have been found in Pennsylvania can be raised as well as other questions relating to geographical location and biological diversity. See http://www.dcnr.state.pa.us/topogeo/education/es2.pdf
    • For students going beyond the standards:
    • Have students develop a geologic time line showing when scientists think that Pangaea broke up, when Gondwanaland and Laurasia formed, and when Gondwanaland separated into the continents as we know them today. See the Related Resources section for Web sites providing more information.
    • The work of Wegener and Du Toit provided the foundation for the theory of plate tectonics, which was developed in the 1960s. What other information came to light that helped scientists develop this theory? Make a poster showing the progression of discoveries and name the scientists who were involved. Use the Web sites in the Related Resources section, as well as earth science textbooks, to find more information.
    • For students requiring more practice with the standards, the following accommodations can be implemented:
    • Have pieces and notes cut out and available for students beforehand.
    • Have questions available or on overhead for students to have in front of them so they can have a visual copy for themselves to look at and process.
    • Let students do the research and maps on a computer.
    • Break lesson up into a three- or four-day unit with more explanation and time for students to process and understand vocabulary and standards of Pangaea and Gondwanaland.

Related Instructional Videos

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DRAFT 11/19/2010
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