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Chapter 10: Iapetus and Pangea

Chapter 10: Iapetus and Pangea

pp. 192-209

Authors

, University of Houston, , McMaster University, Ontario
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Summary

In Chapter 5 we introduced the evidence that at the end of the Paleozoic Era most of the Earth’s continents were joined together, forming the supercontinent Pangea, which in Latin translates as “whole mother-Earth land.” The formation of the Atlantic and Indian oceans primarily records the subsequent breakup of Pangea and led to the hypothesis of continental drift. Although continental drift seemed like a viable mechanism to create new oceans, until we had a full understanding of the Wadati–Benioff subduction zones, where oceans were being destroyed (see Chapter 5), it was reasonable to consider alternate hypotheses.

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