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 3: Drifting Continents and Spreading Seas

Guide to Reading

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This chapter sets the stage for an explanation of plate tectonics, which is explained in detail in Chapter 4. In a sense, this chapter is also setting the stage for the rest of the text, because plate tectonics theory, a relative newcomer to geologic thought, supplies the fundamental explanation for so many geologic processes that it has become a unifying principle in the modern study of geology.

The author begins by drawing a picture of Alfred Wegener who, in the early 1900s, proposed the idea of continental drift, the idea that the continents have moved around in relation to one another. His arguments in support of continental drift include:

  • the fit of the continents
  • paleoclimatic studies that showed evidence of past glaciation, coal deposits, ancient reef deposits, ancient sand dunes, and salt beds that make no sense in today's world climate belts
  • the occurrence of the same fossils on lands now separated by oceans
  • the matching of geologic units (distinct assemblages of rocks) on lands now separated by oceans
For several reasons, Wegener's ideas were not accepted for decades. First, although he was a scientist, he was not a geologist. Second, accepting his ideas would have meant huge changes in geologic thought. And third, he couldn't supply an explanation of how and why continents moved. New discoveries after his death eventually proved that continents do move. The new areas of study involved:

  • changes in the earth's magnetic field over time (paleomagnetism)
  • changes in the sea floor, the shape of its surface, types and ages of its rock, heat flow within it, and sea floor earthquakes, all of which support the idea of sea floor spreading
The author spends considerable time developing a historical context for the theory of plate tectonics. Why? Because:

  • Working through the reasons for accepting new theories, such as the meaning and significance of paleomagnetism, provides practice in good scientific thinking.
  • The gradual acceptance of plate tectonics theory provides an excellent example of the process by which scientific knowledge advances as new evidence and better instruments and techniques are introduced.
  • Plate tectonics was a revolutionary idea that caused profound changes in the study of geology and thus merits your thoughtful study and understanding.

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