B1-2 The Supercontinent of Pangaea
Wegener’s own reconstruction of Pangaea from the 1929 edition of his book alongside a modern version of Pangaea.

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.