Alfred Wegener proposed the theory of continental drift in the early 20th century because he observed similar plant and animal fossils on continents that are now far apart, as well as matching geological formations and evidence of ancient climates that suggest the continents were once joined together and have since drifted apart.
Alfred Wegener was looking at maps once, (as he was a weatherman) and found the edges of each continents fit together like a puzzle. He researched it, and then came up with the theory of Continental Drift. The people did not accept his theory, and asked what made the continents move. He thought that that was not his problem, but the people of the world's problem.
There are currently seven continents on Earth: Africa, Antarctica, Asia, Europe, North America, Australia, and South America.
The land mass that made up all the continents is called Pangaea. It was a supercontinent that existed millions of years ago before the continents drifted apart to their current positions.
The Earth's continents are a result of tectonic plate movements over millions of years, leading to the current configuration of seven main landmasses. These continents have been shaped by geological processes such as continental drift, volcanic activity, and erosion. The number of continents is a human-made concept based on how we divide and categorize the Earth's landmasses.
he had no proof how the continents drifted or what made them drift
Alfred Wegener.
1) Most scientists did not believe Wegener's theory and thought it was foolish.] Some critics thought the old theories of giant land bridges could explain the similarities among fossils in South America and Africa. Others argued that Wegener's theory did not explain the forces that would have been needed to move continents to such great distances. Wegener thought that the forces that moved the continents could be the same forces that made earthquakes and volcanic eruptions.
One question Alfred Wegener could not answer was the mechanism that caused the movement of continents, as he proposed the theory of continental drift before the discovery of plate tectonics. He could not explain how or why continents would be able to move through solid oceanic crust.
Alfred Wegener observed that the continents seemed to fit together like pieces of a puzzle, that identical fossils and rock formations were found on separate continents, and that similar climates and geological features occurred on continents that were now far apart. These observations led him to propose the theory of continental drift.
Alfred Wegener proposed the theory of continental drift in the early 20th century because he observed similar plant and animal fossils on continents that are now far apart, as well as matching geological formations and evidence of ancient climates that suggest the continents were once joined together and have since drifted apart.
Alfred Wegener used several lines of evidence to support his theory of continental drift, including the fit of the continents like pieces of a jigsaw puzzle, similarities in rock formations and fossils across continents, as well as evidence of past glaciation patterns and ancient climate belts that only made sense if the continents were once connected.
It was Alfred Wegener but other scientists did not believe him but he found evidence
because they believed god made the world as it is, and it was perfect.
His theory stated that only continents move, we later found that plates are made of ocean pieces too, not just land masses.
Alfred Wegener, a German scientist, was one of the first to propose the theory of continental drift in the early 20th century. He suggested that all continents were once part of a single supercontinent called Pangaea and had drifted to their current positions over time.
Many geologists and scientists at the time made fun of Alfred Wegener's Drift Theory, dismissing it as implausible and unscientific. Wegener's theory of continental drift proposed that the continents were once connected and drifted apart over time, which was not widely accepted until much later when the theory of plate tectonics was formulated.