Alfred Wegeners 1912 theory of Plate tectonics and continental drift.
Yes
Wegener's theory of continental drift was different because it proposed that continents were once joined together in a supercontinent called Pangaea and drifted apart over time. This was a radical idea at the time as it challenged the established belief of stationary continents. Wegener lacked a plausible mechanism to explain how continents moved, which led to skepticism from the scientific community until the development of plate tectonics theory.
Alfred Wegener, a German meteorologist and geophysicist, presented the theory of continental drift in 1912. His theory was later supported by evidence from paleontology, geology, and geophysics, leading to the development of the theory of plate tectonics.
Many scientists dismissed the theory because it flew in the face of conventional wisdom.
There was no evidence to prove it
yes it does.
Fossils support his hypothesis.
Alfred Wegeners 1912 theory of Plate tectonics and continental drift.
It was not excepted because they didn't believe him at all until it was proven!
plate tectonics
The Continental Drift theory is a theory because there is no evidence to support it. Alfred Wegener developed the Continental Drift theory in the 1800's.
One weakness of Wegener's proposal of continental drift was the lack of a mechanism to explain how continents could move. Additionally, Wegener's theory was not widely accepted at the time due to insufficient supporting evidence and the reluctance of the scientific community to accept such a radical idea.
why did other scientist not accpet Alfred Wegeners theory
While geological research during the sixties had shed new light into the theory, it was J. Tuzo Wilson's proposal of a mechanism for continental drift what led to widespread acceptance of the theory. Proposing a feasible mechanism was something Wegener himself had failed to do, he had only proposed some evidence (complementary Coastlines and fossil distributions across continents.) and falsified mechanisms (like Earth's centrifugal pseudoforce).
The discovery of mid-ocean ridges and the process of seafloor spreading in the 1960s caused scientists to rethink Wegener's theory of continental drift. This new evidence provided a mechanism for how continents could move apart and lent support to the concept of plate tectonics as the driving force behind the movement of Earth's lithospheric plates.
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