On January 06, 1912, German geologist Alfred Wegener presented his theory of continental drift for the first time in public at a meeting of the Geological Society (‘Geologische Vereinigung’) at Senckenberg Museum in Frankfurt, Germany.
Alfred Wegener was born in Berlin, Germany, as the youngest of five children to his father, Richard Wegener, a theologian and teacher of classical languages at the Berlinisches Gymnasium zum Grauen Kloster. In 1886 his family purchased a former manor house near Rheinsberg, which they used as a vacation home. The young Alfred Wegener’s interest in nature evolved during the time he spent with his family in Rheinsberg where they kept a summer house. He was enabled an adequate education and studied physics, meteorology, and astronomy in Berlin, Heidelberg, and Innsbruck before writing his dissertation in Berlin in astronomy. From 1902 to 1903 during his studies he was an assistant at the Urania astronomical observatory. He obtained a doctorate in astronomy in 1905 based on a dissertation written under the supervision of Julius Bauschinger at Friedrich Wilhelms University, Berlin. Wegener had always maintained a strong interest in the developing fields of meteorology and climatology and his studies afterwards focused on these disciplines.After these achievements, he gained his interest in meteorology and physics.
In 1905 Wegener became an assistant at the Aeronautisches Observatorium Lindenberg near Beeskow. He worked there with his brother Kurt, two years his senior, who was likewise a scientist with an interest in meteorology and polar research. The two pioneered the use of weather balloons to track air masses. On a balloon ascent undertaken to carry out meteorological investigations and to test a celestial navigation method using a particular type of quadrant (“Libellenquadrant”), the Wegener brothers set a new record for a continuous balloon flight, remaining aloft 52.5 hours from April 5–7, 1906.
The first expedition, Alfred Wegener took part in was Greenland, led by the Danish researcher Ludvig Mylius-Erichsen, in 1906. Their goal was to explore the last unknown parts of Greenland’s northern coast, but unfortunately, Mylius-Erichsen died during the expedition along with two further team members. Wegener was able to construct the first meteorological station near Danmarkshavn, now able to measure the arctic climate. After the expedition, Wegener used his new material for books and lectures he was widely admired for, due to his ability to deliver complex research results comprehensible and exact. It was also in this period, when Wegener openly began talking about his theory of continental drift.
In the early 1910’s, Wegener left for another expedition to Greenland, achieving major scientific results concerning meteorology and geology. On 6 January 1912 he publicized his first thoughts about continental drift in a lecture at a session of the Geologischen Vereinigung at the Senckenberg-Museum, Frankfurt am Main and in three articles in the journal Petermanns Geographische Mitteilungen. Alfred Wegener first thought of this idea by noticing that the different large landmasses of the Earth almost fit together like a jigsaw puzzle. The Continental shelf of the Americas fit closely to Africa and Europe, and Antarctica, Australia, India and Madagascar fitted next to the tip of Southern Africa. He analyzed both sides of the Atlantic Ocean for rock type, geological structures and fossils. He noticed that there was a significant similarity between matching sides of the continents, especially in fossil plants.
After returning from his Greenland expedition, Wegener had to take part in World War I, but was still highly motivated to bring forward his documentation on the continental drift theory through his work ‘Die Entstehung der Kontinente und Ozeane‘ (“The Origin of Continents and Oceans”, 1915). However, due to the happenings during the war, only few people gained much interest in Wegener’s major work and his many publications in this field of study.
It was in the 1920’s, when his continental drift theory found some interested researchers, but what they had to contribute was not quite, what Wegener wished to hear. At first he heard much criticism from German fellow scientists and later internationally. Until then, the occurrences of certain fossiles on various continents was explained with the famous land-bridge hypothesis. It meant that former individuals moved on these isthmuses from one continent to another, contrary to the Wegener’s theory. But fortunately Wegener was after years of hard work almost completely able to prove his theory though many observations. He explained the similarity of India’s, Madagascar’s, and East-Africa’s rock formation and how the precambrian rocks of Scotland resembled the one’s at Labrador across the Atlantic Ocean. His evidences went on in the field of paleontology and climate-observations.
While Wegener’s theories remained controversial throughout his lifetime, various scientists continued their interest in the field and a few, for instance the geophysicists Maurice Ewing and Edward C. Bullard or the American geologist Harry Hess openly defended Alfred Wegener’s statements. A few years later, the scientific knowledge concerning satellite geodesy grew and through the new research field, his theory could by finally and completely proved.
Alfred Wegener died in Clarinetania, Greenland, in the course of his forth and last Greenland expedition, in November 1930, at age 50.
At yovisto academic video search, you may enjoy an ‘Alfred Wegener Medal Lecture‘ by Michael Ghil at the 2012 General Assembly of the European Geosciences Union.
References and Further Reading:
-  [In German] Alfred Wegener Biography by Alfred-Wegener-Institut für Polar- und Meeresforschung in der Helmholtz-Gemeinschaft [PDF]
-  [In German] Gerhart Wagner: Haareis – eine seltene winterliche Naturerscheinung. Was haben Pilze damit zu tun? [PDF]
-  Alfred Wegener Institut Website
-  Alfred Wegener, Die Entstehung der Kontinente und Ozeane – full digital facsimile at Linda Hall Library
-  Alfred Wegener at Wikidata