Evidence of ancient climates, such as glacial deposits in regions that are now near the equator, support continental drift theory because they suggest that these regions were once located at higher latitudes where glaciers were common. This is consistent with the idea that continents were once joined together in different configurations and have since drifted to their current positions. Additionally, similarities in fossil distributions and rock formations across continents also support the theory of continental drift.
Fossil evidence of plants and animals that were once distributed across continents and matching geological formations such as mountain ranges or rock layers on different continents provide clues supporting the continental drift hypothesis. Additionally, evidence of past climates, such as ancient glacial deposits in regions that are now far from the poles, further support the idea of continental drift.
Wegener showed evidence of similar rock formations and mountain ranges on different continents, evidence of matching plant and animal fossils on different continents, evidence of matching glacial deposits on different continents, and evidence of matching ancient climates on different continents to support his theory of continental drift.
Fossil similarities across continents. Matching geological formations across continents. Alignment of mountain ranges across continents. Distribution of ancient climates and glacial deposits.
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.
Alfred Wegener used a variety of evidence to support his theory of continental drift, including the jigsaw-like fit of continents, matching rock formations and fossils across continents, and similarities in ancient climates and geological structures. He did not have access to modern technology such as GPS or satellite imagery.
Fossil evidence of plants and animals that were once distributed across continents and matching geological formations such as mountain ranges or rock layers on different continents provide clues supporting the continental drift hypothesis. Additionally, evidence of past climates, such as ancient glacial deposits in regions that are now far from the poles, further support the idea of continental drift.
Wegener showed evidence of similar rock formations and mountain ranges on different continents, evidence of matching plant and animal fossils on different continents, evidence of matching glacial deposits on different continents, and evidence of matching ancient climates on different continents to support his theory of continental drift.
Fossil similarities across continents. Matching geological formations across continents. Alignment of mountain ranges across continents. Distribution of ancient climates and glacial deposits.
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.
Alfred Wegener used a variety of evidence to support his theory of continental drift, including the jigsaw-like fit of continents, matching rock formations and fossils across continents, and similarities in ancient climates and geological structures. He did not have access to modern technology such as GPS or satellite imagery.
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.
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.
Which type of evidence was NOT used by Alfred Wegener to support his continental drift hypothesis human remains
Evidence supporting continental drift includes the fit of the continents like pieces of a giant jigsaw puzzle, matching geological features across different continents, similarities in rock formations and mountain chains, distribution of fossils across continents, and the pattern of magnetic stripes on the ocean floor that support seafloor spreading. These pieces of evidence collectively support the theory of continental drift proposed by Alfred Wegener.
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.
The pieces of evidence Alfred Wegener used to support his theory about continental drift were; Puzzle Fit, Fossil evidence from animals that were once on the same continent, geologic evidence like mountain chains that were connected and now split apart, and ice sheets. Thank you for reading this article and I hoped it answered your question!
Alfred Wegener used several lines of evidence to support his theory of continental drift, including the jigsaw-like fit of the continents, similarities in rock formations and fossil remains across continents, and the matching geological features along coastlines of different continents, such as mountain ranges and ancient glacial deposits.