Wegener used evidence from fossils, rock formations, and the fit of the continents as key components to develop his theory of continental drift. By studying these factors, he proposed the idea that all continents were once part of a single supercontinent called Pangaea.
Alfred Wegener used fossil evidence, particularly the presence of identical plant and animal fossils on continents that are now separated by oceans, to develop the theory of continental drift. This suggested that those continents were once joined together.
Alfred Wegener was a German scientist who was the first one to discover the continental drift. In 1915, Alfred Wegener, suggested that about 300 million years ago all of Earth's land masses, which were in constant motion, collided to form one supercontinent. He called it Pangaea , which means " all land". About 200 million years ago, the supercontinent of Pangaea started to break up. The pieces drifted in different directions to their present positions. Wegener had 4 proofs for his theory of continental drift. Most scientists did not accept the theory because Wegener could not explain what force was powerful enough to move continents. Wegener tried to prove his theory: He saw the jigsaw fit between South America and Africa. He found fossils of the same plants and animals on both continents. He believed that they exist in both places only if the continents were once joined together. It was not until the 1960's that the technology existed to develop Wegener's theory further. By 1968, a new and more complete theory known as plate tectonics had been developed.
Alfred Wegener used evidence from the fit of continents, similarities in rock types and structures, fossil evidence, and ancient climate data to develop his theory of Pangaea. He also considered the distribution of plant and animal species across continents to support his idea of continental drift.
Alfred Wegener did not develop the theory of climatic regions. He is, however, known for proposing the theory of continental drift, suggesting that Earth's continents were once joined together as a single landmass called Pangaea. This idea laid the foundation for the modern theory of plate tectonics.
Wegener used evidence from fossils, rock formations, and the fit of the continents as key components to develop his theory of continental drift. By studying these factors, he proposed the idea that all continents were once part of a single supercontinent called Pangaea.
Alfred Wegener was the first person to fully develop a theory that all the continents of the world were once part of the same giant landmass (or supercontinent) called Pangea; which broke apart with the constituent parts drifting away from one another and arriving at their current locations. This drift is still occurring today and some scientists believe that the continents will eventually recombine to form another supercontinent called Pangaea ultima.
Alfred Wegener used fossil evidence, particularly the presence of identical plant and animal fossils on continents that are now separated by oceans, to develop the theory of continental drift. This suggested that those continents were once joined together.
The observation that led Alfred Wegener to develop the hypothesis of continental drift was that the continents looked like a puzzle that could fit together and then found out that fossils of similar kind and whats left of similar plants were found on opposite sides of the world.
One of His Theorys of continental drift was, that you could fit the continents back together if you had pictures. Also it would make up Pangea
Alfred Wegener was a German scientist who was the first one to discover the continental drift. In 1915, Alfred Wegener, suggested that about 300 million years ago all of Earth's land masses, which were in constant motion, collided to form one supercontinent. He called it Pangaea , which means " all land". About 200 million years ago, the supercontinent of Pangaea started to break up. The pieces drifted in different directions to their present positions. Wegener had 4 proofs for his theory of continental drift. Most scientists did not accept the theory because Wegener could not explain what force was powerful enough to move continents. Wegener tried to prove his theory: He saw the jigsaw fit between South America and Africa. He found fossils of the same plants and animals on both continents. He believed that they exist in both places only if the continents were once joined together. It was not until the 1960's that the technology existed to develop Wegener's theory further. By 1968, a new and more complete theory known as plate tectonics had been developed.
Alfred Wegener noticed that the outlines of the continents seemed to fit together like pieces of a jigsaw puzzle, particularly the coastlines of South America and Africa. This observation led him to develop the theory of continental drift.
Alfred Wegener used evidence from the fit of continents, similarities in rock types and structures, fossil evidence, and ancient climate data to develop his theory of Pangaea. He also considered the distribution of plant and animal species across continents to support his idea of continental drift.
hotspots on the ocean floor
Yes, Wegener did use evidence of glacial striations to support his theory of continental drift. He observed that matching glacial striations on continents separated by oceans suggested they were once connected and had moved apart. This was one of the pieces of evidence Wegener used to develop his theory of plate tectonics.
Alfred Wegener did not develop the theory of climatic regions. He is, however, known for proposing the theory of continental drift, suggesting that Earth's continents were once joined together as a single landmass called Pangaea. This idea laid the foundation for the modern theory of plate tectonics.
I believe his first observation was the way the continents of South America and Africa "fit" together like a jigsaw puzzle (although he was not the first to realize this). He also made note of fossil discoveries in Africa which corresponded to those in South America. Finally, he began his own research which actually alligned rock formation/componants from one side of the Atlantic with the other.