Wegener formalized his theory of continental drift in his 1915 book The Origins of Continents and Oceans. Wegener stated that over 200 million years ago, an original supercontinent had existed that he called Pangaea. Pangaea broke apart into many smaller segments. These individual segments moved or drifted over time until they formed the shape and location of the current continental landmasses.
The topographic fit of continents was only one piece of evidence that Wegener used to support his theory of continental drift. Topographic fit, however, had been dismissed by most scientists as just a curiosity and a coincidence. Wegener himself only became convinced of the reality of continental drift as a result of other evidence he found to support his theory. Other forms of evidence that he presented to support continental drift included: geologic evidence, fossil evidence, and climate evidence.
Wadi El-Hitan (Arabic for “Valley of Whales) is located in the Egyptian desert about 150 kilometres southwest of Cairo.
Wadi El-Hitan is significant because of its large concentration of nearly intact fossilized whale skeletons. These whale fossils are estimated to be between 34 and 40 million years old. Wadi El-Hitan was designated a UNESCO World Heritage site in 2005 because of the quality and the number of its unique fossils.