Wegener's continental drift hypothesis posited the existence of a single super landmass called "Pangaea." This supercontinent existed during the late Paleozoic and early Mesozoic eras, approximately 335 to 175 million years ago, before it began to break apart into the continents we recognize today. Wegener suggested that the continents were once joined together and gradually drifted apart over geological time.
Wegener's hypothesis for continental drift, proposed in the early 20th century, suggests that continents were once part of a single supercontinent called Pangaea, which gradually broke apart and drifted to their current positions. He based his hypothesis on evidence such as the fit of continental coastlines, similar geological features across continents, and fossil correlations. Despite presenting compelling evidence, Wegener's theory was initially met with skepticism due to the lack of a mechanism to explain how continents could move. It wasn't until the development of the theory of plate tectonics that his ideas gained widespread acceptance.
The hypothesis that continents have moved is called continental drift. This theory suggests that Earth's continents were once joined in a single supercontinent called Pangaea and have since moved apart to their current positions.
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.
Continental drift is the hypothesis that states that the continents once formed a single land
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.
Wegener's hypothesis for continental drift, proposed in the early 20th century, suggests that continents were once part of a single supercontinent called Pangaea, which gradually broke apart and drifted to their current positions. He based his hypothesis on evidence such as the fit of continental coastlines, similar geological features across continents, and fossil correlations. Despite presenting compelling evidence, Wegener's theory was initially met with skepticism due to the lack of a mechanism to explain how continents could move. It wasn't until the development of the theory of plate tectonics that his ideas gained widespread acceptance.
The hypothesis that continents have moved is called continental drift. This theory suggests that Earth's continents were once joined in a single supercontinent called Pangaea and have since moved apart to their current positions.
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.
The hypothesis of continental drift suggests that continents were once joined together in a single landmass called Pangaea and have since drifted apart to their current positions. This theory was proposed by Alfred Wegener in the early 20th century and is supported by evidence such as matching geological formations, fossils, and the fit of continental coastlines.
A part of the Pangaea hypothesis is called continental drift, which suggests that the Earth's continents were once connected in a single landmass before breaking apart and drifting to their current positions.
Continental drift is the hypothesis that states that the continents once formed a single land
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.
The hypothesis that proposed that Earth's continents were once joined in a single land mass is called continental drift. This theory, formulated by Alfred Wegener in the early 20th century, suggested that the continents were once part of a supercontinent called Pangaea that later broke apart and drifted to their current positions.
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.
Well it wasn't so much climate as the fossils that have been found. Fossils have been found in Antarctica of plants that only occur in tropical climates so at one point it must have had a tropical climate. That is the most dramatic example but there are more subtle ones that led him to believe that the continents, at one point, must have been in different locations on the Earth and then moved to where they currently are.
this supercontinent is called PANGEA. it is the greek word for "all lands".
Because identical fossils were found on two continents far apart, it suggested that at one time the two landmasses were joined together. In other cases of lands separated by far less distance, plants did not propagate across the divide.