Figure 28 Heat flows from Earth's hot interior toward the cooler surface mainly through large convection currents in the mantle. Plates are the uppermost part of a global convection system.

A cross section of the Earth to show the convection current that takes place in the mantle. It also shows the lithosphere, outer and inner core and the mantle.

The process that drives plate movement on Earth's surface is similar to convection in a pot of boiling soup. The soup is heated from below and rises to the top of the pot, moves across the top and cools, and then sinks back down.

The heat that drives convection in the mantle comes from two sources. Earth was very hot when it first formed, and some of the heat moving upward in convection currents is due to the gradual cooling of its interior. A second source of heat is the result of the decay of radioactive isotopes that are distributed throughout the mantle and crust.


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Table of Contents

Physical Science CHAPTER 1 Science Skills CHAPTER 2 Properties of Matter CHAPTER 3 States of Matter CHAPTER 4 Atomic Structure CHAPTER 5 The Periodic Table CHAPTER 6 Chemical Bonds CHAPTER 7 Chemical Reactions CHAPTER 8 Solutions, Acids, and Bases CHAPTER 9 Carbon Chemistry CHAPTER 10 Nuclear Chemistry CHAPTER 11 Motion CHAPTER 12 Forces and Motion CHAPTER 13 Forces in Fluids CHAPTER 14 Work, Power, and Machines CHAPTER 15 Energy CHAPTER 16 Thermal Energy and Heat CHAPTER 17 Mechanical Waves and Sound CHAPTER 18 The Electromagnetic Spectrum and Light CHAPTER 19 Optics CHAPTER 20 Electricity CHAPTER 21 Magnetism CHAPTER 22 Earth's Interior CHAPTER 23 Earth's Surface CHAPTER 24 Weather and Climate CHAPTER 25 The Solar System CHAPTER 26 Exploring the Universe Skills and Reference Handbook