plate tectonics
Alfred Wegener's hypothesis of continental drift proposed that the Earth's continents were once joined together in a single supercontinent called Pangaea. He suggested that over time, Pangaea broke apart and the continents drifted to their current positions. Wegener supported this theory with evidence like matching coastlines, similar rock formations, and fossil distribution across continents.
The main objection to Wegener's hypothesis of continental drift was the lack of a plausible mechanism to explain how continents could move. Wegener's idea of continents plowing through solid oceanic crust was not supported by scientific knowledge at that time, leading many scientists to reject his hypothesis.
Alfred Wegener proposed the continental drift hypothesis in 1912, suggesting that continents were once connected in a supercontinent called Pangaea and drifted to their current positions. Despite facing skepticism initially, his ideas laid the foundation for the theory of plate tectonics, which explains the movement of Earth's lithosphere.
Alfred's hypothesis was that all the continents were a big land mass which he called Pangaea because if you see a world map it is like a jigsaw puzzle and other evidence is that some animal fossils were on other continents. Also the same rock range was found on different continents.
Alfred Wegener proposed the hypothesis of continental drift, suggesting that the continents were once joined together in a single landmass called Pangaea. He proposed that the continents had drifted apart over time to their current positions. This idea laid the foundation for the theory of plate tectonics.
All of the continents fit together like a puzzle.
the continents were once joined together in a single landmass
They all fit together like a puzzle.
Alfred Wegener proposed the theory of continental drift, suggesting that continents were once joined together in a single supercontinent called Pangaea. Over time, the supercontinent broke apart and the continents drifted to their current positions, explaining why they seem to fit together like pieces of a puzzle.
A super continent called Pangaea.
Alfred Wegener's hypothesis of continental drift proposed that the Earth's continents were once joined together in a single supercontinent called Pangaea. He suggested that over time, Pangaea broke apart and the continents drifted to their current positions. Wegener supported this theory with evidence like matching coastlines, similar rock formations, and fossil distribution across continents.
Wegener's hypothesis of continental drift proposed that continents were once joined together in a single landmass called Pangaea and have since drifted apart over time. This theory laid the foundation for the modern theory of plate tectonics, which explains the movement of Earth's lithosphere.
The main objection to Wegener's hypothesis of continental drift was the lack of a plausible mechanism to explain how continents could move. Wegener's idea of continents plowing through solid oceanic crust was not supported by scientific knowledge at that time, leading many scientists to reject his hypothesis.
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The man who pioneered the continental drift hypothesis was Alfred Wegener. He proposed the theory in 1912, suggesting that Earth's continents were once joined together in a single landmass called Pangea and have since drifted apart.
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.
Alfred Wegener proposed the continental drift hypothesis in 1912, suggesting that continents were once connected in a supercontinent called Pangaea and drifted to their current positions. Despite facing skepticism initially, his ideas laid the foundation for the theory of plate tectonics, which explains the movement of Earth's lithosphere.