Maybe the depth of oceans
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.
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.
he used fossils, glacial indentations, and different types of rock.
Fossils of similar plants and animals found on separate continents, such as the Mesosaurus and Glossopteris, provide evidence for continental drift. Additionally, matching geological formations and mountain ranges on different continents support the theory of continental drift. Magnetic striping on the ocean floor also supports the movement of continents over time.
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.
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 evidence from the fit of continents, distribution of fossils, rock types, and ancient climate data to support his theory of continental drift.
human remains
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.
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.
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.
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.
Fossils of similar plants and animals found on separate continents, such as the Mesosaurus and Glossopteris, provide evidence for continental drift. Additionally, matching geological formations and mountain ranges on different continents support the theory of continental drift. Magnetic striping on the ocean floor also supports the movement of continents over time.
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.
We find matching types of ancient fossils separated on coinciding land masses across the Atlantic Ocean, where Brazil would abut Africa.
The hypothesis of continental drift was proposed by Alfred Wegener in 1912 to explain the jigsaw-like fit of continents, similarities in rock types and fossils, and paleoclimate data. It wasn't widely accepted until the 1960s when evidence from paleomagnetism and seafloor spreading supported the theory.