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 2: Journey to the Center of the Earth

Guide to Reading

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Chapter 1 dealt with the long ago and far way, presenting theories about the origin and development of the Universe. Chapter 2 brings you into the present and much closer to home with an overview and an inner view of planet Earth. It starts miles high above Earth in the vacuum of interplanetary space, then zooms down through Earth's magnetic field, magnetosphere, and Van Allen radiation belts, pausing in the upper atmosphere to comment on the obvious topography of Earth and the great amount of hydrosphere covering Earth's surface. The journey continues, diving down below the ocean surface and progressing through Earth's crust, mantle, and core.

Much of the chapter deals with the ocean bottom and inner earth, as preparation for plate tectonics theory, presented in Chapters 3 and 4. The author discusses Earth's composition (organic chemicals, minerals, glasses, rocks, metals, melts, and volatiles) and layers (oceanic and continental crust, the Moho, oceanic and continental lithosphere, asthenosphere, upper mantle, transition zone, lower mantle, outer core, and inner core.)

Few humans have visited the ocean bottom, and no human has physically been more than 2 miles below Earth's land surface. How do we know what it's like inside the Earth? Your author describes scientists' efforts to reach deep into Earth and discusses the various approaches and scientific reasoning that have provided answers to questions about composition, structure, and conditions within Earth. These include the use of clues obtained from measuring Earth's density and shape, the study of earthquake (seismic) wave velocities, and meteorites.

There are lots of terms and many numbers involved in this survey of Earth. Try not to get mired down in lists of rock types or thickness of layers. Instead concentrate on the thought processes necessary to analyze something you can neither see nor touch and on the truly amazing world that exists under your feet. Jules Verne's fanciful journey to the center of the Earth of the 1800s was tame compared to the real thing. He imagined exotic versions of environments on Earth's surface, all places within the realm of human experience, transposed to its interior. The real interior of Earth is beyond any human's experience. It's a place of awesome pressures and temperatures, much closer than the stars but just as unreachable. Truth can certainly be stranger than fiction.

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