Alfred Wegener facts for kids

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Alfred Wegener
Alfred Wegener ca.1924-30.jpg
Alfred Wegener, about 1925
Born 1 November 1880
Died 13 November 1930
Nationality German
Alma mater University of Berlin
Known for continental drift
Scientific career
Fields meteorology
Gondwana fossil map ger
Fossil records suggesting that continents now separated were once together: see Pangaea
Antonio Snider-Pellegrini Opening of the Atlantic
First known illustration of the opening of the Atlantic Ocean, by Antonio Snider-Pellegrini, 1858.
Alfred-Wegener-Gedenktafel, Wallstraße 42, Berlin-Mitte, 533-639
Commemorative plaque on Wegener's former school in Wallstrasse

Alfred Lothar Wegener (1 November 1880 – 13 November 1930) was a German scientist and meteorologist. He is most notable for his theory of continental drift, which he proposed in 1912. This was the idea that the continents were slowly drifting around the Earth. At the time he was unable to demonstrate a mechanism for this movement, and other scientists thought it was simply impossible. His hypothesis was not accepted until the 1950s when several discoveries gave evidence of continental drift.

Wegener was born in Berlin and in 1904 he earned his PhD in Astronomy at the University of Berlin. In 1914 he was drafted ('called up') into the German Army. After he was severely wounded he was transferred to the army weather service.

Plate tectonics theory

The theory had been proposed before, more than once. The first time was by the mapmaker Abraham Ortelius in the 16th century.

Wegener's theory

Wegener used geologic, fossil, and glacial evidence from opposite sides of the Atlantic Ocean to support his theory of continental drift. For example, he said that there were geological similarities between the Appalachian Mountains in North America, and the Scottish Highlands. Also, he said that the rock strata in South Africa and Brazil were similar.

He believed these similarities could be explained only if these geologic features were once part of the same continent. Wegener said that because they are less dense, continents float on top of the denser rock of the ocean floor. Although continental drift explained many of Wegener's observations, he could not find scientific evidence to make a complete explanation of how continents move.


The British geologist Arthur Holmes championed the theory of continental drift at a time when it was deeply unfashionable. He proposed in 1931 that the Earth's mantle contained convection cells that dissipated radioactive heat and moved the crust at the surface. His Principles of Physical Geology, ending with a chapter on continental drift, was published in 1944.

However, most Earth scientists and palaeontologists did not believe Wegener's theory and thought it was foolish. Some critics thought the old theories of giant land bridges could explain the similarities among fossils in South America and Africa. Others argued that Wegener's theory did not explain the forces that would have been needed to move continents to such great distances. Wegener thought that the forces that moved the continents could be the same forces that made earthquakes and volcanic eruptions.


During the 1950s, in the mid-atlantic ridge discoveries of sea-floor spreading and magnetic reversal proved that Wegener's theory was real and led to the theory of plate tectonics. Today geologists say that continents are actually parts of moving tectonic plates that float on the asthenosphere, a layer of partly molten rock.

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