Evidence supporting continental drift includes the distribution of fossils and rock formations that match across continents, the fit of continental coastlines like puzzle pieces, and the alignment of mountain ranges and geological structures across continents. Additionally, the matching of ancient climates and glacial deposits across separate continents supports the theory of continental drift.
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.
Matching geological features across continents, such as rock formations and mountain ranges. Fossil evidence of similar species found on separate continents. Alignment of coastlines and identical climate indicators in regions that are now widely separated. Distribution of plant and animal species that suggests they were once connected. Paleoclimatic evidence, such as glacial deposits in regions that are now too warm for glaciers.
One type of evidence for continental drift is fossil evidence, such as plant and animal fossils that are found on separate continents but are closely related. Another type is geological evidence, including the matching of rock formations and mountain ranges on different continents, as well as the distribution of earthquakes and volcanoes along continental boundaries.
Yes, fossil evidence such as similar plant and animal species found on separate continents has been used to support the continental drift hypothesis. The distribution of fossils across continents suggests that these land masses were once connected and later moved apart.
Paleoclimatic evidence supporting continental drift includes the matching of certain rock formations, geological structures, and fossil distribution on continents now separated by vast oceans. For example, the presence of glacial deposits and coal seams that match across continents provides evidence that these landmasses were once connected. Additionally, the alignment of ancient climatic belts and the distribution of certain plant and animal species further support the theory of continental drift.
Evidence for continental drift includes the fit of the continents like a puzzle, similarities in rock formations and fossils across continents, and matching mountain ranges and geologic structures on different landmasses. Additionally, the distribution of certain species and climate indicators supports the theory of continental drift. These pieces of evidence suggest that the continents were once connected and have since moved apart over millions of years.
Part 1: Evidence from the Fossil Record Part 2: Evidence from Geographic Distribution of Living Species Part 3: Evidence from Homologous Structures and Vestigial Organs Part 4: Evidence from Embryology
The same fossils found on different sides of the ocean.
Wegener's data included evidence from fossil similarities between continents, matching mountain ranges and geological features across continents, similar rock sequences, and the distribution of ancient climates and glaciations.
Evidence supporting continental drift includes the distribution of fossils and rock formations that match across continents, the fit of continental coastlines like puzzle pieces, and the alignment of mountain ranges and geological structures across continents. Additionally, the matching of ancient climates and glacial deposits across separate continents supports the theory of continental drift.
Part 1: Evidence from the Fossil RecordPart 2: Evidence from Geographic Distribution of Living SpeciesPart 3: Evidence from Homologous Structures and Vestigial OrgansPart 4: Evidence from Embryologymore: What_are_the_four_pieces_of_evidence_for_evolution
Alfred Wegener used evidence from the fit of continents, similarities in rock types and structures, fossil evidence, and ancient climate data to develop his theory of Pangaea. He also considered the distribution of plant and animal species across continents to support his idea of continental drift.
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.
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.
The geographic distribution of the swimming reptile Mesosaurus provides evidence that supports continental drift. Fossils belonging to the Mesosaurus were found far away from each other, in both South Africa and South America.
Evidence supporting the hypothesis of continental drift includes the fit of continental coastlines, matching rock formations and fossils across continents, and the alignment of mountain ranges. Additionally, the distribution of ancient glacial deposits and paleoclimate data further support the idea that continents were once connected.