Plate tectonics and Pangaea you get evidence from ancient climate zones, land features, and fossils
Rock types can provide evidence of continental drift by matching on opposite sides of current oceans, showing that the continents were once connected. For example, the Appalachian Mountains in North America align with the Caledonian Mountains in Scotland, indicating they were once part of the same mountain range before continental drift occurred. Additionally, similar fossils and rock formations found on different continents support the theory of continental drift.
Climate patterns and fossil evidence can help support continental drift theory. For example, matching rock formations and fossils across continents suggest they were once connected. Additionally, similarities in climate types and geological features between distant landmasses also provide evidence for past continental connections.
No, Alfred Wegener did not use paleomagnetism in his theory of continental drift. Wegener's theory was based on evidence from fossil records, geological formations, and similarities in rock types and mountain ranges on different continents. Paleomagnetism became a significant piece of evidence supporting continental drift theory after Wegener's time.
Evidence for continental drift includes matching geological formations on different continents, such as mountain ranges and sedimentary layers. Additionally, the fit of the continents like puzzle pieces, similarities in fossil records on separate continents, and matching glacial evidence provide support for the theory. Paleoclimatic evidence, such as the distribution of ancient flora and fauna, also contributes to the case for continental drift.
Continental Drift was put forward by Alfred Wegener.(1880-1930). One piece of evidence on which he based his ideas was the similarity of shapes of the South American and African coastlines. Another was the fact that the same types of fossil are found in both places.
human remains
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.
Rock types can provide evidence of continental drift by matching on opposite sides of current oceans, showing that the continents were once connected. For example, the Appalachian Mountains in North America align with the Caledonian Mountains in Scotland, indicating they were once part of the same mountain range before continental drift occurred. Additionally, similar fossils and rock formations found on different continents support the 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.
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.
Wetness data included sediment and rock formations, fossil evidence of past climates and species, and the distribution of certain minerals and rock types across different continents. This evidence supported the theory of continental drift by indicating past connections between landmasses now separated by oceans.
Climate patterns and fossil evidence can help support continental drift theory. For example, matching rock formations and fossils across continents suggest they were once connected. Additionally, similarities in climate types and geological features between distant landmasses also provide evidence for past continental connections.
No, Alfred Wegener did not use paleomagnetism in his theory of continental drift. Wegener's theory was based on evidence from fossil records, geological formations, and similarities in rock types and mountain ranges on different continents. Paleomagnetism became a significant piece of evidence supporting continental drift theory after Wegener's time.
Evidence for continental drift includes matching geological formations on different continents, such as mountain ranges and sedimentary layers. Additionally, the fit of the continents like puzzle pieces, similarities in fossil records on separate continents, and matching glacial evidence provide support for the theory. Paleoclimatic evidence, such as the distribution of ancient flora and fauna, also contributes to the case for continental drift.
Continental Drift was put forward by Alfred Wegener.(1880-1930). One piece of evidence on which he based his ideas was the similarity of shapes of the South American and African coastlines. Another was the fact that the same types of fossil are found in both places.
he used fossils, glacial indentations, and different types of rock.
The five pieces of evidence for Wegener's continental drift theory are: (1) the fit of the coastlines of continents like South America and Africa, (2) the distribution of similar fossils and rock types on different continents, (3) the alignment of mountain ranges across continents, (4) the presence of ancient glacial deposits in tropical regions, and (5) paleoclimatic evidence such as coal beds in Antarctica.