Shape, fossil animals and plants, magnetic field reversals, residual magnetic fields of rocks, subduction zones.
Three pieces of evidence used to prove the theory of continental drift were the fit of the continents' coastlines, the distribution of fossils across continents, and the matching geological formations found on separate continents. These observations supported the idea that the continents were once joined together and had drifted apart over time.
Evidence such as the distribution of fossils, rock formations, and magnetic fields on different continents support the theory of continental drift and the breakup of Pangaea. The matching geological features, such as mountain ranges and coastlines, on opposite sides of the Atlantic Ocean provide further evidence that the continents were once connected. Additionally, the movement of tectonic plates and the ongoing process of plate tectonics help explain the separation of the continents from Pangaea.
Fit of continents: The edges of continents like South America and Africa fit together like puzzle pieces. Fossil evidence: Similar fossils of plants and animals found on different continents suggest they were once connected. Rock formations: Matching rock formations and mountain ranges across continents support the idea of continental drift. Paleoclimate data: Evidence of past climates, such as glaciers in regions that are now tropical, can be explained by continental drift. Seafloor spreading: Mid-ocean ridges and magnetic striping on the seafloor provide evidence of tectonic plate movement and support the theory 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.
Alfred Wegener proposed the theory of Pangaea based on the fit of the continents, similarities in rock formations, and fossil evidence across continents. He also noted similarities in geological structures and climate data that suggested the continents were once connected before drifting apart. However, Wegener's theory was not widely accepted until much later when additional evidence and advancements in plate tectonics supported his ideas.
Two main pieces of evidence that support Wegner's theory of continental drift are the fit of the continents' coastlines, indicating they were once connected, and the distribution of similar fossils and rock formations across separate continents, suggesting a shared geological history.
Three pieces of evidence used to prove the theory of continental drift were the fit of the continents' coastlines, the distribution of fossils across continents, and the matching geological formations found on separate continents. These observations supported the idea that the continents were once joined together and had drifted apart over time.
Alfred Wegener proposed three main pieces of evidence for his hypothesis of continental drift. First, he noted the jigsaw-like fit of continents, particularly South America and Africa, suggesting they were once joined. Second, he identified similar geological formations and fossil remains across widely separated continents, indicating they were once connected. Lastly, he pointed to paleoclimatic evidence, such as glacial deposits in now tropical regions, which suggested that continents had shifted over time to their current locations.
Evidence such as the distribution of fossils, rock formations, and magnetic fields on different continents support the theory of continental drift and the breakup of Pangaea. The matching geological features, such as mountain ranges and coastlines, on opposite sides of the Atlantic Ocean provide further evidence that the continents were once connected. Additionally, the movement of tectonic plates and the ongoing process of plate tectonics help explain the separation of the continents from Pangaea.
Fit of continents: The edges of continents like South America and Africa fit together like puzzle pieces. Fossil evidence: Similar fossils of plants and animals found on different continents suggest they were once connected. Rock formations: Matching rock formations and mountain ranges across continents support the idea of continental drift. Paleoclimate data: Evidence of past climates, such as glaciers in regions that are now tropical, can be explained by continental drift. Seafloor spreading: Mid-ocean ridges and magnetic striping on the seafloor provide evidence of tectonic plate movement and support the theory 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.
to put them together like a puzzle or to look at the fossils that are found in 3 different continents
Alfred Wegener proposed the theory of Pangaea based on the fit of the continents, similarities in rock formations, and fossil evidence across continents. He also noted similarities in geological structures and climate data that suggested the continents were once connected before drifting apart. However, Wegener's theory was not widely accepted until much later when additional evidence and advancements in plate tectonics supported his ideas.
The fact that there are subduction zones where continental plates meet !
Alfred Wegener used geological and paleontological evidence to propose the theory of continental drift. He observed similarities in rock formations, fossils, and mountain ranges on different continents that suggested they were once connected. Additionally, Wegener developed a hypothesis known as Pangaea, suggesting a supercontinent that gradually broke apart over millions of years to form the continents we see today.
Well, the main answer to this question are the fossils. Since fossils were found in different parts of the world and those fossils are of the same breed or species. Because having the same species in different locations are quite... Unusual, Alfred Wegener developed this theory. Searching for other evidences to prove his theory, he found that pieces of land from another place to another fit's perfectly like a piece of puzzle. This is the second answer to this question.
Fossil evidence of the same species found on separate continents. Geological similarities between distant continents, such as matching rock formations or mountain ranges. Distribution of ancient glacial deposits that suggest a former connection. Similarities in plant and animal species distribution across continents. Continuity of similar geological structures beneath the continental shelves.