Pangaea was the name given by Alfred Wegener to the supercontinent that existed during the late Paleozoic and early Mesozoic eras, approximately 335 to 175 million years ago. He proposed that Pangaea was a single landmass that eventually broke apart, leading to the current distribution of continents. Wegener's hypothesis of continental drift suggested that the continents were once joined together before drifting to their current positions. This idea laid the groundwork for the modern theory of plate tectonics.
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.
Alfred Wegener, a German meteorologist, proposed the theory of continental drift in the early 20th century. Wegener's hypothesis suggested that the Earth's continents were once joined together in a single supercontinent called Pangaea and have since drifted apart. Although initially met with skepticism, his work laid the foundation for the development of the theory of plate tectonics.
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.
Wegener's theory of continental drift assumed the existence of one original supercontinent called Pangaea.
continental drift
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.
Alfred Wegener proposed the hypothesis of continental drift in 1912, suggesting that the continents were once joined in a supercontinent he called Pangaea. His idea laid the groundwork for the development of the theory of plate tectonics.
Pangaea was the supercontinent into which all the land masses were concentrated until about 200 million years ago.
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.
Alfred wegener
A super continent called Pangaea.
Yes
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.
His hypothesis of continental drift
Which type of evidence was NOT used by Alfred Wegener to support his continental drift hypothesis human remains
Alfred Wegener, a German meteorologist, proposed the theory of continental drift in the early 20th century. Wegener's hypothesis suggested that the Earth's continents were once joined together in a single supercontinent called Pangaea and have since drifted apart. Although initially met with skepticism, his work laid the foundation for the development of the theory of plate tectonics.