Chapter 14 discusses the continental drift hypothesis, initially proposed by Alfred Wegener, which suggests that continents are in constant motion and were once part of a supercontinent called Pangaea. Evidence for this theory includes the apparent fit of continents, fossil similarities across continents, and geological correlations between mountain ranges. Despite presenting substantial evidence, Wegener's ideas faced skepticism due to a lack of explanation for the mechanisms behind continental movement, which were not understood until the discovery of plate tectonics.