Wegener Presents Continental Drift Theory
In the early 20th century, scientists largely accepted fixed continents separated by sunken land bridges to explain similar fossils and rock formations across oceans. On January 6, 1912, German meteorologist and geophysicist Alfred Wegener delivered his first public lecture on continental drift to the German Geological Society in Frankfurt. He proposed that continents had once formed a supercontinent and had slowly drifted apart over geological time, supported by matching coastlines, geological structures, and fossil evidence. The presentation occurred just before Wegener departed for another Greenland expedition. His ideas challenged prevailing geological orthodoxy.
