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Unit 6: Dynamic Planet: Plate Tectonics Lecture 3

Earth's Interior. The original surface of the Earth probably looked much as the Moon's surface does today. The Earth was probably composed of the same material from its surface all the way to its center.Objects colliding with Earth helped to cause Earth to grow hot enough that heavy elements such

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Unit 6: Dynamic Planet: Plate Tectonics Lecture 3

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    1. Unit 6: Dynamic Planet: Plate Tectonics Lecture 3 Objectives: E3.2C - Describe the differences between oceanic and continental crust (including density, age, composition). E3.r3e - Predict the temperature distribution of the lithosphere as a function of distance from the mid-ocean ridge and how it relates to ocean depth.

    2. Earth’s Interior

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