Alfred Lothar Wegener proposed his theory of continental drift in 1912.
The idea of Pangaea, the supercontinent that existed during the late Paleozoic and early Mesozoic eras, was first proposed by the German meteorologist Alfred Wegener in 1912. He suggested that continents were once joined together and have since drifted apart, a concept he called "continental drift." Wegener's theory was initially met with skepticism but laid the groundwork for the development of plate tectonics in the mid-20th century.
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There were several reasons. First, Wegener's ideas were quite radical, and many scientists probably found the idea of continents moving absurd. Second, he lacked a plausible explanation for how the continents might move. Third, Wegener was a meteorologist, not a geologist, so most geologists would not be inclined to trust his judgement on matters of geology.
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The matching coastlines or jigsaw puzzle-like fit of the continents, as well as the fossil and rock formations that span across continents, suggested to early cartographers the concept of continental drift or the idea that the continents were once joined together in a single supercontinent. This idea eventually led to the development of the theory of plate tectonics.
The idea of continents moving is known as the theory of plate tectonics, and it was proposed by Alfred Wegener in the early 20th century. Wegener suggested that continents were once joined together in a supercontinent called Pangaea and have since drifted apart.
wegener
The man who proposed the idea that the seven continents were once joined together is Alfred Wegener. He introduced the theory of continental drift in the early 20th century, suggesting that the continents were once part of a single supercontinent called Pangaea. This idea laid the groundwork for the modern theory of plate tectonics.
Alfred Wegener proposed the theory of continental drift in the early 20th century. He suggested that the continents were once joined together in a single supercontinent called Pangaea and have since drifted apart. This idea eventually led to the development of the theory of plate tectonics.
One main evidence is the fit of the continents' coastlines, particularly the fit of South America and Africa. Fossil evidence of similar species found on different continents also supports the idea of continental drift. Additionally, the matching geological features and rock formations across continents provide further evidence for the theory of continental drift.
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.
The idea of continental drift was first proposed by Alfred Wegener in 1912. He suggested that the continents were once joined together in a single supercontinent called Pangaea and have since drifted apart.
this supercontinent is called PANGEA. it is the greek word for "all lands".
Wegener's theory of continental drift proposed that the continents were once joined together in a single supercontinent called Pangaea. Over time, the continents drifted apart to their current positions. This idea eventually led to the development of the theory of plate tectonics, which explains the movement of Earth's lithosphere on the underlying asthenosphere.
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.
Alfred Wegener came up with the idea of Pangaea by observing the fit of South America and Africa's coastlines, as well as similarities in rock formations and fossils on different continents. He proposed the theory of continental drift to explain how the Earth's landmasses were once joined together in a supercontinent called Pangaea before drifting apart over time.