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Alfred Wegener was unable to prove his theory about Pangaea because he lacked a mechanism to explain how continents could move across the Earth's surface. Additionally, Wegener's theory was met with skepticism from the scientific community at the time due to the lack of supporting evidence and alternative explanations being more widely accepted. It wasn't until the development of the theory of plate tectonics in the 1960s that Wegener's ideas were finally validated.
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 proposed the theory of continental drift, suggesting that Earth's continents were once joined together in a single landmass called Pangea and have since drifted apart. His theory was rejected because he could not provide a plausible mechanism for how the continents could move across the ocean floor. It was not until the discovery of plate tectonics that Wegener's ideas were accepted and incorporated into the scientific understanding of Earth's geology.
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.
Alfred Wegener used evidence from fossil records, similarities in rock formations across continents, and matching geological features as evidence to support his theory of Pangaea. These observations led him to propose the idea of continental drift, suggesting that the continents were once joined together as a single landmass.