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∙ 11y agofossils
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∙ 11y agoAnimals
fossils
The same rocks and minerals from the same batch, dinosaur fossils dating back to the same time periods, natural landforms and structures can be found on completely separate continents. This evidence supports the Plate Techtonics and Continental Drift theories.
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.
They were separated, like a giant island, from the rest of the world. They didn't really welcome outsiders. They didn't even know there was more in the world than them. They didn't think there were other people living in different continents. They thought that they were located on the middle of Earth. That's why they are referred to as "The Middle Kingdom". Hope it helps!
Alfred Wegener noticed that the coastlines of continents appeared to fit together like a jigsaw puzzle and found similar rock formations and fossils on different continents. He proposed the Continental Drift Theory by suggesting that all continents were once part of a single supercontinent called Pangaea, which later broke apart and drifted to their current positions over millions of years.
Alfred Wegener and others noticed that the shapes of continents seemed to fit together like pieces of a jigsaw puzzle, similar fossils and rock formations appeared on different continents, and evidence of past climates that were not possible in current locations. These observations led them to hypothesize that the continents had moved over time, which eventually became the theory of plate tectonics.
Alfred Wegener studied the concept of Pangaea, the supercontinent that existed millions of years ago, by examining the fit of continents, the distribution of fossils, and rock formations across different continents. He proposed the theory of continental drift to explain how the continents had once been joined together and later drifted apart.
Alfred Wegener, a German meteorologist and geophysicist, first proposed the theory of continental drift in the early 20th century. He noticed the puzzle-like fit of the continents, suggesting that they were once joined together in a single landmass he 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 did not use evidence of climate change in his theory of continental drift. Instead, he proposed that continents were once connected and later drifted apart based on geological evidence like the fit of continents, matching rock layers, and similar fossils found on different continents.
Alfred Wegener used the fit of the continents, fossil evidence, and rock formations to support his theory of continental drift. He noticed how the continents seemed to fit together like a jigsaw puzzle, found similar fossils on different continents, and discovered matching rock layers across continents. These pieces of evidence led him to propose the idea of Pangaea and the movement of continents over time.