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 his theory of continental drift based on three main pieces of evidence: first, the jigsaw-like fit of continental coastlines, particularly South America and Africa; second, the presence of similar fossils, such as Mesosaurus and Glossopteris, found on widely separated continents; and third, geological similarities, including matching rock formations and mountain ranges across continents. These observations suggested that continents were once connected and have since drifted apart over time.
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.
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 proposed his theory of continental drift by citing three main pieces of evidence: first, the jigsaw-like fit of the continents, particularly South America and Africa; second, the distribution of similar fossils across widely separated continents, such as the Mesosaurus found in both South America and Africa; and third, geological similarities, including matching rock formations and mountain ranges found on different continents. These observations suggested that the continents were once joined together in a supercontinent before drifting apart.
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 used several pieces of evidence to support his theory of continental drift, including the fit of continents like South America and Africa, similar rock formations and mountain ranges across continents, and the distribution of plants and animals. He also looked at evidence from fossils and ancient climate data to support his hypothesis.
Alfred Wegener used fossil evidence, geological evidence, paleoclimatic evidence, and the fit of continental coastlines to support his theory of continental drift. By comparing fossils, rock formations, climate patterns, and the alignment of continents like puzzle pieces, Wegener proposed that the continents were once connected in a single supercontinent called Pangaea that drifted apart over time.
Matching geological formations across continents. Fossil evidence of similar species on different continents. Similar ancient climates and rock formations across continents. Fit of the continents like puzzle pieces on the Earth's surface.
Wegener's continental drift hypothesis was supported by several lines of evidence, including the fit of the continents, fossil correlations, and geological similarities across continents. For instance, the distribution of similar fossil species, such as Mesosaurus, found in both South America and Africa, suggested that these continents were once connected. Additionally, the alignment of mountain ranges and rock formations across continents indicated a shared geological history. These pieces of evidence collectively bolstered Wegener's argument for the movement of continents over time.
Alfred Wegener gathered several pieces of evidence to support his continental drift hypothesis, including the fit of the continents, matching geological formations across different continents, similarities in fossil distributions, and paleoclimatic evidence such as glacial deposits and coal seams in regions that are now separated by oceans. These pieces of evidence suggested that the continents were once connected and have since drifted apart.
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.
seafloor spreading, age of the sea floor and ocean trenches.
South America and Africa fit together like puzzle pieces.
Yes, Wegener did use evidence of glacial striations to support his theory of continental drift. He observed that matching glacial striations on continents separated by oceans suggested they were once connected and had moved apart. This was one of the pieces of evidence Wegener used to develop his theory of plate tectonics.
True. Alfred Wegener, the scientist who proposed the theory of continental drift, used the distribution of fossils of tropical plants across continents as evidence to support his idea that the continents were once connected. This was one of the key pieces of evidence Wegener used to support his theory.
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.