Alfred Wegener's theory of continental drift was supported by several lines of evidence, including the matching Coastlines of different continents, similarities in rock formations and mountain ranges across continents, and the distribution of fossils of similar species on different continents. He also observed the fit of the continents like pieces of a jigsaw puzzle and the presence of ancient glacial deposits in regions that are now at different latitudes.
Alfred Wegener used several pieces of evidence to support his theory of continental drift, including the fit of continents like South America and Africa, similarities in rock formations and fossils across continents, and the matching of ancient climate indicators like glaciation patterns. Despite facing initial skepticism, Wegener's evidence paved the way for the development of the theory of plate tectonics.
Alfred Wegener proposed the theory of Continental Drift in 1912.
Alfred Wegener did not use direct geological evidence, such as rock samples or detailed seismic data, to support his theory of continental drift. Instead, he relied on indirect evidence like the fit of continental coastlines, the distribution of fossils across continents, and the similarities in rock formations and mountain ranges on different continents.
Many geologists and scientists at the time made fun of Alfred Wegener's Drift Theory, dismissing it as implausible and unscientific. Wegener's theory of continental drift proposed that the continents were once connected and drifted apart over time, which was not widely accepted until much later when the theory of plate tectonics was formulated.
Alfred Wegener presented several pieces of evidence to support his theory of continental drift, including the jigsaw-like fit of continents, particularly South America and Africa. He also noted the similarity of fossil remains, such as the Mesosaurus, found on widely separated continents, and similarities in rock formations and mountain ranges across continents. Additionally, he observed climatic evidence, like glacial deposits in now-tropical regions, which suggested that continents had once been positioned differently.
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.
Alfred Wegener used fossil evidence, geological evidence, and paleoclimatic evidence to support his theory of Continental Drift. Fossils of the same species found on different continents, similar rock formations and mountain ranges across continents, and matching ancient climate patterns were key pieces of evidence that he presented.
Alfred Wegener used various pieces of evidence to support his theory of continental drift, including the fit of the continents, rock and fossil similarities across continents, glacial evidence, and similar geological features on different continents.
No, Alfred Wegener proposed the theory of continental drift, not a shrinking earth. He used evidence from matching coastlines, fossils, rock types, and climate to support his idea that the continents were once joined in a single supercontinent called Pangaea.
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No, Alfred Wegener provided evidence from continental drift and fossil distribution to support his theory of plate tectonics, not a shrinking Earth. Wegener's theory suggested that the continents were once connected in a single landmass (Pangaea) and drifted apart over time due to the movement of tectonic plates.
Frederick J. Vine helped Alfred Wegener by providing important evidence to support the theory of continental drift. Vine's research on magnetic anomalies in the ocean floor provided crucial support for Wegener's idea of plate tectonics. This collaboration helped to further validate Wegener's revolutionary theory in the field of geology.
Alfred Wegener used evidence such as the fit of the continents, matching geological formations across continents, identical fossil species found on different continents, and similarities in rock types and mountain ranges as support for his theory of continental drift.
Alfred Wegener
he used fossils, glacial indentations, and different types of rock.
Alfred Wegener used evidence such as the apparent fit of the continents, similarities in rock formations and mountain ranges across continents, and the distribution of fossils of identical species in continents that are now separated by vast oceans to support his theory of the breakup of Pangaea. He also cited geological and paleontological evidence from different continents that suggested they were once connected.
Alfred Wegener had discovered pangaea in the year of 1912.