Wagner proposed the theory of continental drift, suggesting that the continents were once joined together in a single supercontinent called Pangaea. He observed that identical rock sequences and geological structures appeared on different continents, supporting the idea of continental movement over time.
Alfred Wegener believed in continental drift because he observed geological and fossil evidence that suggested the continents were once connected. He noted similarities in rock formations, fossils, and coastlines across different continents, which led him to propose the theory of Pangaea.
Wegener noticed that the continents appeared to fit together like a jigsaw puzzle, especially when looking at the coastlines of South America and Africa. He also observed similarities in rock formations, fossils, and mountain ranges across continents that suggested they were once connected. This led Wegener to propose the theory of continental drift.
Alfred Wegener noticed that the continents looked like they could fit together like a puzzle, particularly along their coastlines. This observation led him to propose the theory of continental drift, suggesting that the continents were once joined together in a supercontinent called Pangaea.
Wegener believed in the theory of continental drift because he noticed that the coastlines of continents seemed to fit together like pieces of a puzzle. He also found similarities in rock formations and fossils across different continents, suggesting they were once connected. These observations led him to propose that the continents were once part of a single supercontinent called Pangaea.
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.
Alfred Wegener proposed the theory of continental drift after observing that the rock sequences and fossil assemblages on different continents matched up when they were thought to have been part of a single supercontinent. He suggested that the continents were once connected and had drifted apart over time.
Alfred Wegener believed in continental drift because he observed geological and fossil evidence that suggested the continents were once connected. He noted similarities in rock formations, fossils, and coastlines across different continents, which led him to propose the theory of Pangaea.
These observations were used in the process of making observations and forming a hypothesis about continental drift. By noticing the fit of continents, matching fossils, and similar structures across different continents, scientists were able to propose the theory that continents were once connected and have since drifted apart. This hypothesis was then tested and supported through further research and evidence gathering.
Wegener noticed that the continents appeared to fit together like a jigsaw puzzle, especially when looking at the coastlines of South America and Africa. He also observed similarities in rock formations, fossils, and mountain ranges across continents that suggested they were once connected. This led Wegener to propose the theory of continental drift.
Alfred Wegener noticed that the continents looked like they could fit together like a puzzle, particularly along their coastlines. This observation led him to propose the theory of continental drift, suggesting that the continents were once joined together in a supercontinent called Pangaea.
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Wegener's theory of continental drift proved the theory of Pangea (all continents as one land mass).
Wegener believed in the theory of continental drift because he noticed that the coastlines of continents seemed to fit together like pieces of a puzzle. He also found similarities in rock formations and fossils across different continents, suggesting they were once connected. These observations led him to propose that the continents were once part of a single supercontinent called Pangaea.
Alfred Wegener, a German meteorologist and geophysicist, proposed the idea of continental drift in 1912. He suggested that the continents were once connected and had since drifted apart, challenging the prevailing belief in stationary continents.
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.
Alfred Wegener proposed the theory of continental drift in 1912, suggesting that the continents had once been part of a single supercontinent called Pangaea. He suggested that the continents slowly drifted apart over millions of years due to the movement of the Earth's tectonic plates.
Alfred Wegner had 4 theory`s,Climate evidence,Fossil evidence,the continents fitting together like a puzzle,and horizontal movement. The fossils were different types of ancient ferns and Dinosaurs.