Astronomy and Space Sciences

CONTENTS OF CURRICULUM UNIT 05.04.03

  1. Unit Guide
  1. Introduction
  2. Student Population
  3. Objectives
  4. Overview
  5. Teaching Strategies
  6. BackgroundContent
  7. Volcanoes in the Solar System
  8. Volcanoes on Earth
  9. Radioactivity
  10. Pangaea
  11. Plate Tectonics
  12. Volcanic Landforms
  13. Volcanoes in Space
  14. Io and Its Volcanoes
  15. Types of Volcanoes on Io
  16. Comparing Volcanoes: Earth and Io
  17. Lesson Plans
  18. Lesson 1: Radioactive Decay
  19. Lesson 2: A Scissor Cut: Snipping away at the Decay Process
  20. Lesson 3 Making and Mapping a Volcano
  21. Lesson 4: Galilean Satellites
  22. Annotated Bibliography
  23. Appendix

Volcanoes in the Solar System

Mary Jefferson

Published September 2005

Tools for this Unit:

Volcanoes on Earth

Planet Earth

Our Earth is the third planet in the Solar System. Scientist has found that the Earth is divided into a solid inner core (700 miles thick) and an outer liquid core (1360 miles thick) at its center. The core is overlain by another layer of less dense material called the mantle. A thin rocky crust (between 3 and 43 miles) overlays the mantle (1800 miles thick). (Rogers, Howell, et al.,180). This is the part upon which man lives. A good example to model this concept is an apple. Zeilinga de Boer and Sanders say that if an apple is sliced into two, the cross section reveals a small, circular "core" (where the seeds are), a thick "mantle" (the edible flesh), and a "crust" (the very thin skin). Those parts of the apple are relatively proportional to the main parts of the Earth. I will have students illustrate the parts of the Earth by using a peach or an egg as the physical model, which shows a more accurate correlation. Students will locate and place a copy of a labeled diagram of the Earth's structure in their cumulative science notebook.

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