Alfred Wegener used geological and paleontological evidence to propose the theory of continental drift. He observed similarities in rock formations, fossils, and mountain ranges on different continents that suggested they were once connected. Additionally, Wegener developed a hypothesis known as Pangaea, suggesting a supercontinent that gradually broke apart over millions of years to form the continents we see today.
Alfred Wegener proposed that the continents of South America and Africa looked like they could fit together like puzzle pieces to form a single landmass called Pangaea.
If the continents were once connected, similarities in coastline features could include similar shapes, geological structures, and fossil evidence of past connections. Additionally, the coastlines might have similar trends or patterns that suggest common tectonic history.
Alfred Wegener proposed the theory of continental drift because he observed evidence such as similar geological features, matching rock layers, and identical fossils on continents that are now widely separated. Wegener suggested that these observations could be explained by the continents drifting apart over millions of years.
Alfred Wegener noticed that the continents looked like they could fit together like a puzzle, particularly along their coastlines. This observation led him to propose the theory of continental drift, suggesting that the continents were once joined together in a supercontinent called Pangaea.
Alfred Wegener proposed that Africa and South America looked like they could fit together like puzzle pieces, supporting his theory of continental drift.
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 believed in continental drift because he observed similarities in rock formations, fossils, and ancient climates across continents that could only be explained by the continents moving over time. He proposed the theory of "Pangaea" to explain how the continents were once connected and drifted apart.
because they had no way of explaing how the continents could move
Observations of a map of the continents hinted that the continents once fitted together. Later, he would discover fossil evidence to support his theory. But alas, he was unable to explain the mechanism by which the continents could move, and was soundly thrashed by geologists of his time. The discoveries leading to the science of plate tectonics were not made until the mid twentieth century.
Alfred Wegner thought that all the continents used to be one giant landmass called Pangea. He said that the continents would move a little each year. The scientists didnt believe him though, but later found out that it could be true because of the plates in the earth
Alfred Wegener proposed the theory of Pangaea based on the fit of the continents, similarities in rock formations, and fossil evidence across continents. He also noted similarities in geological structures and climate data that suggested the continents were once connected before drifting apart. However, Wegener's theory was not widely accepted until much later when additional evidence and advancements in plate tectonics supported his ideas.
Alfred Wegener hypothesized that the continents were once connected in a single supercontinent called Pangaea. He suggested that the continents drifted apart over millions of years due to the process of continental drift.
No he was not. If he was how could he have predicted that the continents were once together
Alfred Wegener proposed that the continents of South America and Africa looked like they could fit together like puzzle pieces to form a single landmass called Pangaea.
Alfred Wegener and others noticed that the shapes of continents seemed to fit together like pieces of a jigsaw puzzle, similar fossils and rock formations appeared on different continents, and evidence of past climates that were not possible in current locations. These observations led them to hypothesize that the continents had moved over time, which eventually became the theory of plate tectonics.
Alfred Wegener used climate to support his hypothesis of continental drift by noting that matching plant and animal fossils, as well as rock formations, across continents with similar past climates suggested that these landmasses were once connected. He argued that the distribution of certain geological features and fossils could only be explained by the movement of the continents over time.
If the continents were once connected, similarities in coastline features could include similar shapes, geological structures, and fossil evidence of past connections. Additionally, the coastlines might have similar trends or patterns that suggest common tectonic history.