Continental drift, proposed by Alfred Wegener in 1912, was initially rejected due to a lack of a plausible mechanism to explain how continents could move across the Earth's surface. Wegener's ideas conflicted with the prevailing geophysical theories of the time, and he could not provide sufficient evidence for the forces driving continental movement. Additionally, his theory was met with skepticism from many geologists who favored static models of the Earth's crust. It wasn't until the development of plate tectonics in the mid-20th century, which provided a comprehensive framework and evidence for continental movement, that Wegener's ideas gained acceptance.
Alfred Wegener
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.
The geologist who first proposed the theory of continental drift was Alfred Wegener. He introduced the concept in 1912, suggesting that continents were once connected and have since drifted apart over geological time. Wegener's ideas were initially met with skepticism, but they laid the groundwork for the later development of plate tectonics. His evidence included the fit of continental margins, fossil similarities, and geological formations across continents.
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.
Alfred Wegener, a German meteorologist and geophysicist, first proposed the theory of continental drift in 1912. He suggested that the continents were once part of a single supercontinent called Pangaea, which later broke apart and drifted to their current positions due to the movement of the Earth's mantle caused by thermal convection.
He could not explain how or why the continents moved.
Auther Holmes is the Scientist who first proposed that theral convection in the mantle causes continental drift.
German scientist Alfred Wegener (1880-1930) first proposed the theory of continental drift in 1912, but it was not widely accepted until the 1950s.
Alfred Wegener
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.
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, a German meteorologist and geophysicist, proposed the theory of continental drift in 1912. He suggested that thermal convection currents in the mantle cause the movement of continents over time.
Arthur Holmes
Scientist rejected Wegners hypothesis of continental drift at first because he did not have enogh evidence to support his theory. He failed to provide a suitable mechanism that could cause the continents to move.
A German scientist Alfred Wegener first proposed the idea of Continental Drift.
That would be Alfred Wegener.yah! it's true ALFRED L. WEGENER [1880-1930] who first proposed the CONTINENTAL DRIFT IN 1912. obejerojamjam@yahoo.com :))
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.