The idea of Continental Drift was first proposed by German meteorologist Alfred Wegener in 1912. He suggested that continents were once joined together in a single landmass called Pangaea and have since drifted apart. Wegener's theory was based on evidence from geology, Paleontology, and climatology, although it was not widely accepted until later advancements in plate tectonics provided a mechanism for the movement.
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.
Alfred Wegener is considered the father of the theory of continental drift. In the early 20th century, he proposed the idea that the continents were once connected and had drifted apart over time, forming the basis for the modern theory of plate tectonics.
Alfred Wegener, a German meteorologist, proposed the theory of continental drift in the early 20th century. He suggested that the continents were once part of a single supercontinent called Pangaea that broke apart and drifted to their current positions. Although his ideas were initially met with skepticism, they formed the foundation for the modern theory of plate tectonics.
The theory of continental drift was introduced by German meteorologist Alfred Wegener in 1912. He proposed that the continents were once joined together in a single landmass called Pangea and have since drifted apart to their current positions.
The theory of seafloor spreading was proposed by Harry Hess, a geologist and Navy officer, in the early 1960s. He proposed that new oceanic crust is formed at mid-ocean ridges and then spreads outward. This theory helped to explain the mechanism behind continental drift and plate tectonics.
The idea of continental drift was first proposed by Alfred Wegener in 1912. Wegener's theory suggested that the continents were once joined together in a single landmass called Pangaea and had drifted apart over time.
A German scientist Alfred Wegener first proposed the idea of Continental Drift.
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.
Alfred Wegener was the scientist who proposed the idea of continental drift in the early 20th century. He suggested that the Earth's continents were once joined together in a single supercontinent called Pangaea, which later broke apart and drifted to their current positions.
The German geologist Alfred Wegener first put forward the idea in 1912, but it did not become widely accepted until the 1950s.
Alfred Wegener proposed the theory of continental drift at the beginning of the 20th century. His idea was that the Earth's continents were once joined together, but gradually moved apart over millions of years. The idea was rejected at first as he was a Meteorologist and not regarded as a proper scientist.
Alfred Wegener studied volcanoes. He was a German scientist who proposed the idea of the continental drift.
Alfred Lothar Wegener proposed his theory of continental drift in 1912.
The name of the floral fossils Wegner used for the idea of continental drift was glossopteris. Alfred Wegner used the continental drift as a way to explain the continental shapes.
He proposed the idea of continental dift, which is very cool!
Continental drift is a process that happens so slowly that it is impossible to observe it directly, you can only infer it from various clues. Continents seem to be extremely solid and rooted in place, as far as we can easily observe, so the idea that they move seemed bizarre, when it was first proposed.
The idea that first described the movement of continents is called continental drift. Proposed by Alfred Wegener in the early 20th century, it suggested that Earth's continents were once connected in a supercontinent called Pangaea and have since drifted apart.