1 Cosmology and the Earth
2 Journey to the Center of the Earth
3 Drifting Continents and Spreading Seas
4 The Way the Earth Works: Plate Tectonics
5 Patterns in Nature: Minerals
6 Up from the Inferno: Magma and Igneous Rocks
7 A Surface Veneer: Sediments, Soils, and Sedimentary Rocks
8 Metamorphism: A Process of Change
9 The Wrath of Vulcan: Volcanic Eruptions
10 A Violent Pulse: Earthquakes
11 Crags, Cracks, and Crumples: Crustal Deformations and Mountain Building
12 Deep Time: How Old Is Old?
13 A Biography of Earth
14 Squeezing Power from a Stone: Energy Resources
15 Riches in Rock: Mineral Resources
16 Unsafe Ground: Landslides and Other Mass Movements
17 Streams and Floods: The Geology of Running Water
18 Restless Realm: Oceans and Coasts
19 A Hidden Reserve: Groundwater
20 An Envelope of Gas: Earth’s Atmosphere and Climate
21 Dry Regions: The Geology of Deserts
22 Amazing Ice: Glaciers and Ice Ages
23 Global Change in the Earth System
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Chapter 14: Squeezing Power from a Stone: Energy Resources

Animations

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Click on the links below to view animations created specifically for Earth: Portrait of a Planet. Animations require Macromedia's Flash Plug-in.

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ANIMATION: Oil Formation and Trapping

This animation shows the successive stages in the formation of an oil reserve. In View 1, organic material settles, is buried, and is transformed by heat and pressure into oil. In View 2 an oil trap is formed: the area folds into an anticline, and oil migrates and accumulates in the anticline crest. For more information, see Section 14.3 Oil and Gas starting on p.489 and Figure 14.4 on page 490 in your textbook.

View AnimationZoomable Art: Power from the Earth

Modern society, for better or worse, uses vast amounts of energy to produce heat, to drive modes of transportation, and to produce electricity (see Appendix B). This energy comes either from geologic materials stored in the Earth, or from geologic processes happening at our planet's surface. For more information, see the Featured Painting on pp.514-515 in your textbook.

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