Alfred Wegener used several lines of evidence to establish the theory of continental drift, including the fit of the continents, matching geological features across continents, and the distribution of fossils. One key piece of evidence Wegener used was the matching geological formations and rock types found on different continents, such as the Appalachian Mountains in North America and the Caledonian Mountains in Europe. These similarities in geological features across continents supported Wegener's hypothesis that the continents were once connected and had drifted apart over time.
Alfred Wegener used evidence from the fit of continents, distribution of fossils, rock types, and ancient climate data to support his theory of continental drift.
While Wegner's theory of continental drift assumed that continents plowed through and over oceanic crust, his basic ideas are still upheld today. As a result of submarines and radar technology used in WWII, scientists were better able to map the seafloor. In doing so they discovered the seafloor's topography, age, magnetism, and the Mid-Atlantic Ridge. After discovering that the seafloor did spread apart and that continents moved, Wegner's theory gradually became accepted.
The idea of continental drift has been subsumed by the theory of plate tectonics.
Alfred Wegener's theory of continental drift proposed that all continents were once part of a single supercontinent called Pangaea. Pangaea eventually broke apart into two large landmasses, Laurasia in the north and Gondwana in the south, which later fragmented into the continents we recognize today.
Wegener used evidence from fossils, rock formations, and the fit of the continents as key components to develop his theory of continental drift. By studying these factors, he proposed the idea that all continents were once part of a single supercontinent called Pangaea.
Alfred Wegener used evidence from the fit of continents, distribution of fossils, rock types, and ancient climate data to support his theory of continental drift.
The name of the floral fossils Wegner used for the idea of continental drift was glossopteris. Alfred Wegner used the continental drift as a way to explain the continental shapes.
Wegner used evidence from fossil distributions, rock formations, and the fit of continents like puzzle pieces to support his theory of continental drift. He also noted similarities in plant and animal species found on different continents, suggesting they were once connected.
He used evidence from landform, climate, and fossils to support his theory of the continental drift.
Alfred Wegener used evidence such as the fit of continents like puzzle pieces, matching rock formations and fossils across continents, and similarities in geological features to support his theory of continental drift. These pieces of evidence suggested that the continents were once joined together in a single supercontinent, which later drifted apart to their current positions.
their roots
composition of meteorites
While Wegner's theory of continental drift assumed that continents plowed through and over oceanic crust, his basic ideas are still upheld today. As a result of submarines and radar technology used in WWII, scientists were better able to map the seafloor. In doing so they discovered the seafloor's topography, age, magnetism, and the Mid-Atlantic Ridge. After discovering that the seafloor did spread apart and that continents moved, Wegner's theory gradually became accepted.
Four pieces of evidence used by Alfred Wegener to support his theory of continental drift were the fit of the continents, matching geological formations across continents, similar fossil distributions, and glacial evidence in tropical regions.
The idea of continental drift has been subsumed by the theory of plate tectonics.
Alfred Wegener proposed the idea of continental drift, suggesting that the continents of South America and Africa fit together like a puzzle. He used geological and fossil evidence to support his theory of the supercontinent Pangaea.
Continental drift is a concept relating to the movement of the Earth's continents. The proving of the continental drift theory came from evidence found around the world. Foremost, scientists had discovered that similar plants and animal fossils were found in or around different continents, suggesting that they were once joined. The theory of plate tectonics also supported continental drift. If one were to look at a global map, the complementary arrangements between South America and Africa can be easily seen.