When Alfred Wegener first proposed the continental drift theory in the early 20th century, it was met with skepticism because he did not have a mechanism to explain how the continents moved. Additionally, Wegener's idea challenged long-established geological theories and faced resistance from scientists who were reluctant to accept a new paradigm. It wasn't until the development of the theory of plate tectonics in the 1960s that Wegener's ideas gained widespread acceptance.
Lack of evidence
People initially did not believe Alfred Wegener's continental drift theory because he lacked a mechanism to explain how continents could move across the Earth's surface. Additionally, there was insufficient evidence at the time to support his theory. It was not until the development of the theory of plate tectonics in the 1960s that Wegener's ideas gained widespread acceptance.
Alfred Wegener's theory of continental drift was not initially accepted because he lacked a mechanism to explain how continents could move. Additionally, his evidence was considered insufficient and geologists at that time did not believe that continents could drift over time. It was not until the theory of plate tectonics was developed in the 1960s that Wegener's ideas gained widespread acceptance.
Yes, Alfred Wegener proposed the theory of continental drift to explain the presence of fossil tropical plants in places that now have a polar climate. He argued that these plants must have grown in a different location when the continents were connected and then drifted to their current positions.
Alfred Wegener
Lack of evidence
People initially did not believe Alfred Wegener's continental drift theory because he lacked a mechanism to explain how continents could move across the Earth's surface. Additionally, there was insufficient evidence at the time to support his theory. It was not until the development of the theory of plate tectonics in the 1960s that Wegener's ideas gained widespread acceptance.
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.
Alfred Wegener was a scientist who proposed the theory of continental drift and the idea of isostasy. The idea of isostasy stated that continental blocks drifted upon oceanic blocks (continental blocks had a lower density than oceanic blocks, which explained why it was higher than oceanic blocks).
It was Alfred Wegener but other scientists did not believe him but he found evidence
Alfred Wegener's theory of continental drift was not initially accepted because he lacked a mechanism to explain how continents could move. Additionally, his evidence was considered insufficient and geologists at that time did not believe that continents could drift over time. It was not until the theory of plate tectonics was developed in the 1960s that Wegener's ideas gained widespread acceptance.
Yes, Alfred Wegener proposed the theory of continental drift to explain the presence of fossil tropical plants in places that now have a polar climate. He argued that these plants must have grown in a different location when the continents were connected and then drifted to their current positions.
Alfred Lothar Wegener was a geophysicist and meteorologist. He was born in Berlin, Germany, in 1880 and died in Greenland in 1930. He is known for his advancement with the theory of continental drift in 1912.
Alfred Wegener
Alfred Wegener proposed the theory of Continental Drift in 1912.
Alfred Wegener did not have the "HOW" factor- because of no evidence on the process, they could not believe his theory.
Alfred Wegener grew up in a wealthy family in Berlin, Germany, where he developed a passion for science and nature. He spent much of his childhood exploring the outdoors and dreaming of becoming a polar explorer. Wegener's early experiences and education later influenced his groundbreaking work in the field of geology and continental drift theory.