They all fit together like a puzzle.
Alfred Wegener's hypothesis of continental drift explains that continents were once part of a single supercontinent called Pangea, which over time drifted apart to their current positions. This theory is supported by geological evidence such as the matching shapes of continents on opposite sides of the Atlantic Ocean.
the continents were once joined together in a single landmass
All of the continents 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.
Alfred Wegener couldn't describe how the plate tectonics moved. So, scientists rejected his hypothesis.
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.
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.
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.
A super continent called Pangaea.
His hypothesis of continental drift
Which type of evidence was NOT used by Alfred Wegener to support his continental drift hypothesis human remains
The continental drift hypothesis was proposed by Alfred Wegener, a German meteorologist and geophysicist, in 1912. He suggested that the continents were once joined together in a single landmass called Pangaea and had since drifted apart to their current positions.