Wegener's continental drift theory is supported by several key pieces of evidence, including the jigsaw-like fit of continents, particularly South America and Africa. Fossil evidence shows similar species, such as the Mesosaurus, found on widely separated continents. Additionally, geological formations and mountain ranges, like the Appalachian Mountains and the Caledonian Mountains in Scotland, display striking similarities, indicating they were once part of a single landmass. Lastly, paleoclimatic evidence, such as coal deposits in polar regions and glacial deposits in currently warm areas, suggests continents have shifted over geological time.
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.
Many scientists dismissed the theory because it flew in the face of conventional wisdom.
Seafloor Spreading.
There was no evidence to prove it
yes it does.
Fossils support his hypothesis.
Alfred Wegeners 1912 theory of Plate tectonics and continental drift.
plate tectonics
It was not excepted because they didn't believe him at all until it was proven!
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
rekmr
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.