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Alfred Wegener tried to explain how continental drift took place, but he had no concrete evidence about how the continents moved. He had to explain what force is pushing and pulling the continents. And mainly in the early 1900s, most geologists thought that mountains formed because Earth was slowly cooling and shrinking. So most geologists would have to change their ideas of how mountains formed. Then in 1960 Harry Hess, an American geologist, he thought about the ocean floor in relation to the problem of continental drift. He proposed a process called sea-floor spreading. In sea-floor spreading, the sea floor spreads apart along both sides of a mid-ocean ridge as new crust is added. The ocean floors move like conveyor belts, carrying the continents with them. Hess soon found evidence from molten material, magnetic stripes, and rock samples from the mid-ocean ridges. And he proved that Wegener's theory wasn't wrong.

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Q: Why was wegeners theory ignored until the mid 1960s?
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Was the theory of a 'super continent' originally accepted by scientists?

When German meteorologist Alfred Wegener first published his theory on Pangea (super continent) he was widely ridiculed for it. Some of the reaction to his theory on continental shift and a super continent was actually quite hostile. The idea was first put forward in 1912 but it wasn't until the 1950's that his idea was really rethought. By then evidence of continental drift was starting to support his ideas.


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Is it true that most geologists of wegener's time accepted his idea of drifting continentals?

No, Wegener's theory of continental drift faced significant skepticism and opposition from the scientific community during his time. Many geologists did not accept his idea, as it challenged the prevailing belief in stationary continents. It was not until several decades later, with the discovery of seafloor spreading and the development of plate tectonics theory, that Wegener's ideas gained acceptance and were validated.


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Alfred Lothar Wegener was a geophysicist and meteorologist. He was born in Berlin, Germany, in 1880 and died in Greenland in 1930. He is known for his advancement with the theory of continental drift in 1912.

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